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HomeMy WebLinkAbout20170520 Ver 3 _PCN Application _20180222February 15, 2018 Kinston KINi -TON! PUBLIC SE'JR -ITS'"111 Mft CRY Buildings & Grounds, Business Office, Electric, Engineering, Environmental Services, III I Fleet Maintenance, Meter Reading, Stormwater, Streets, Wastewater, and Water 2009 Kinston, the right place ... Kinston public Srrvims, the right choice Ms. Karen Higgins, Supervisor North Carolina Department of Environment and Natural Resources Water Resources Division 401 and Buffer Permitting Branch 512 North Salisbury Street Archdale Building — 9th floor Raleigh, North Carolina 27604 RE: Response to Comments Waste Water Collection System Improvements Briery Run Sewer Rehabilitation Phase IV City of Kinston Lenoir County Dear Ms. Higgins: Please find enclosed one (1) copy of The Plans, Specifications aPre-Construction Notification (PCN) Form, and supporting documentation which includes Watershed Classification Attachment, Wetlands Evaluation, and The Categorical Exclusion issued by Water Infrastructure for the above referenced project. The Plans and specifications have been revised in response to comments from your November 30, 2017, letter requesting additional information, and this package has also been submitted electronically. Plan Details for stream Impacts: Please enumerate all stream impacts including fill slopes /dissipater pads/ other impacts on the site plan and clearly label impacts (Stream Impact 1, etc.). The division recommends highlighting by hatching or shading all impacts areas for temporary impact areas and permanent impact areas. In addition, please provide cross section details showing the provisions for aquatic life passage. Also, please provide a detailed engineering plan, profile view, and cross-section of all proposed culverts. These drawings must include details regarding stream alignment in relation to pipe alignment, pipe slope, pipe burial, and dissipater pad [15A NCAC 02H .0502(g)(b, and (b)92)] The application form, PCN, Plans and Specifications have been revised as follows: All stream crossings are noted on the Plans and they are enumerated as they are in the application form, PCN. All crossings will be made using Construction Matting as shown on the Plans and described in the Specifications and The Application (PCN form) See Section D1 on Post OKce Box 339 Kinston, North Carolina 28502 Phone (252) 939-3287 Fax (252) 939-3279 page 7 of 12. Construction Matting will be laid on existing grade causing minimal impact to the area. Construction Matting will be temporary and construction matting will not be allowed to stay on the ground through the entire project. See the stream crossing detail which will allow aquatic life to pass over the temporary crossing. No culverts are being proposed. The Stream Crossing Narrative has been revised to include discussion on Buffers and Station Numbers. The Wetland Narrative has been revised to remove any reference to Rip -rap stream crossings. The Plans and the Specifications have also been revised to remove the reference to rip -rap stream crossings. See Sheet 4 of 14, Sheet 5 of 14, Sheet 6 of 14 and Sheet 9 Of 14 of the Plans. Plan Details for buffer impacts: Please enumerate all riparian buffer impacts on the site plan and clearly label impacts (Buffer Impact 1, etc.). The Division recommends highlighting by hatching or shading all impacts areas for temporary areas and permanent impact areas. [15A NCAC 02H .0233(8)(b)(iv)] This project is Exempt from the rule, since it is ongoing activity for maintenance of a sewer installed in 1973 (before July 22, 1997. [15A NCAC 02H .023(3)(b)(i)] However, the City wishes to comply with the rule and maintain the buffer in good faith. The Buffers are noted on the Plan and the Temporary Impact is construction matting through the buffers, and is noted in Section D1 on page 7 of 12.. The Buffers are listed and discussed in the Stream Crossing Narrative, and they are shown on the Plans, See Sheet 4 of 14, Sheet 5 of 14, Sheet 6 of 14 and Sheet 9 Of 14 of the Plans. Any additions which were made to the narratives and the Application (PCN Form), were done in red. I trust that changes made in the application, plans and specifications are adequate for approval. Thank you for your consideration, and we await your approval of the plans. Should you have any questions or comments, please do not hesitate to contact me by phone at (252) 939-3239 or by e-mail at john.iarrell(ii,)ci.kinston.nc.us. ;Sonceregly, hn A. Jarrell, IIIP.E. ty Enineer Enclosures: cc: Mr. Steve Miller, Assistant Director of Public Services Mr. Brian Lucas, Water Resources Manager Mr. Justin Howard, Engineer Mr. Charles Sutton, Inspector Mr. Robert Tankard, Washington Regional Office Supervisor Mr. Anthony Scarbraugh, Washington Regional Office Mr. Gary Beecher, US Army Corps of Engineers, Washington Post OfFce Box 339 Kinston, North Carolina 28502 Phone (252) 939-3287 Fax (252) 939-3279 I_v11iI I� T 'fNl Pel i!E CLIC SE1I�CES1 FUBIIG Buildings & Grounds, Business Office, Electric, Engineering, Environmental Services, Fleet Maintenance, Meter Reading, Stormwater, Streets, Wastewater, and Water Kinston, the nghtplace ... Kinston Puhlic Services, the right choice. Kinston 2009 CITY OF KINSTON �7 E�C��O��l� p���®NSTG3�C�TBON NC�TOG�Oc�nT�ON ��1�M9i�i�,L� FOR P1 ]AGE W ' MIERY RUN OUTFALL SEWER 6' EHABIM T M THE CITY OF F(INSTON SEWER COLLECTION SYSTEM RHONDA BARWICIC, ®IRECTOR OF PUBLIC SERVICES STEVE MILLER, P.E., ASSISTANT DIRECTOR OF PUBLIC SERVICES BRIAN LUCAS, WATER RESOURCES MANAGER JOHN JARRELL, P.E., CITY ENGINEER ii, 1i iii ii ;'� liirgo7k ffwfi BRIERY RUN SEWER REHABILITATION PHASE Iv LIST OF DOCUMENTS 71r1�� 1. PRE -CONSTRUCTION NOTIFICATION (PCN) FORM 12 A. 401 & Buffer Permitting PCN Checklist 3 B. Property and Easement Information 1 C. Project Description (from Erosion and Sediment Control Permit) 2 D. STREAM CROSSING NARRATIVE 6 1. FORM WSCAS, WATERSHED CLASSIFICATION 2 2, USGS MAP of The Project Area 1 3, Briery Run Phase IV Stream Crossing Map 1 4. July 26, 2017 Site determination 2 a. USGS Map of Project Area 1 b. USDA Lenoir County Soils Map of Project Area 1 E. WETLAND NARRATIVE 12 1. Briery Run Phase IV Project Access Map 1 2, Briery Run Phase IV Soils Map 1 3, Briery Run Phase IV Topographical Map 1 F. Neuse River Basin Map 1 G. USGS Topographical Map in a pocket 1 H. NRCS/USDA Soil Map and Survey information 37 I. EREID approval and Categorical Exclusion 3 5. ATTACHMENTS A. Plans 14 Sheets B. Specifications 394 Pages i Office Use Only: Corps action ID no. DWQ project no. Form Version 1.3 Dec 10 2008 Page 1 of 12 PCN Form —Version 1.3 December 10, 2008 Version Pre -Construction Notification (PCN) Form A. Applicant Information 1, Processing 1 a. Type(s) of approval sought from the Corps: X Section 404 Permit X Section 10 Permit 1b. Specify Nationwide Permit (NWP) number: 12 or General Permit (GP) number: 1c. Has the NWP or GP number been verified by the Corps? ❑Yes X No 1d. Type(s) of approval sought from the DWQ (check all that apply): X 401 Water Quality Certification — Regular X Non -404 Jurisdictional General Permit ❑ 401 Water Quality Certification — Express X Riparian Buffer Authorization Is. Is this notification solely for the record because written approval is not required? For the record only for DWQ 401 Certification: ❑ Yes X No For the record only ❑ Yes for Corps Permit: X No 1f. Is payment into a mitigation bank or in -lieu fee program proposed for mitigation of impacts? If so, attach the acceptance letter from mitigation bank or in -lieu fee program. ❑ Yes X No 1g, Is the project located in any of NC's twenty coastal counties. If yes, answer 1 h below. ❑ Yes X No 1 h. Is the project located within a NC DCM Area of Environmental Concern (AEC)? ❑ Yes X No 2. Project Information 2a. Name of project: Briery Run Sewer Rehabilitation Phase IV 2b, County: Lenoir 2c. Nearest municipality I town: Kinston 2d. Subdivision name: N/A 2e. 3. NCDOT only, T.I.P. or state N/A project no: Owner Information 3a. Name(s) on Recorded Deed: See attached Table: "Property and Easement Information" 3b. Deed Book and Page No. See attached Table: "Property and Easement Information" 3c. Responsible Party (for LLC if applicable): City of Kinston, Tony Sears, City Manager 3d. Street address: 207 East King Street 3e. City, state, zip: Kinston, North Carolina, 28501 3f. Telephone no.: (252) 939-3212 3g. Fax no.: (252) 939-3388 3h. Email address: tony.sears(d?ci.kinston.nc.us Page 1 of 12 PCN Form —Version 1.3 December 10, 2008 Version 4. Applicant Information (if different from owner) 4a. Applicant is: ❑ Agent ❑ Other, specify: 4b. Name: 4c. 4d. Business name (if applicable): Street address: 4e. City, state, zip: 4f. Telephone no.: 4g. Fax no.: 4h. Email address: 5. Agent/Consultant Information (if applicable) 5a. Name: John A. Jarrell III, P.E. 5b. Business name (if applicable): City of Kinston, City Engineer 5c. Street address: 2360 Highway 258 South 5d. City, state, zip: Kinston, North Carolina, 28504 5e. Telephone no.: (252) 939-3239 5f. Fax no.: (252) 939-3279 5g. Email address: John, 4arrellOci.kinston.nc.us Page 2 of 12 B. Project Information and Prior Project History 1. Property Identification la. Property identification no. (tax PIN or parcel ID): See attached Table: "Property and Easement Information" 1b. Site coordinates (in decimal degrees): Latitude (See Form WSCAS) Longitude: - START: (35.310537) START: (-77.545717) END: (35.30761) END: (-77.59149) 1c. Property size: 962.29 acres Easement Area = 11.76 acres 2. Surface Waters 2a. Name of nearest body of water (stream, river, etc.) to proposed project: Briery Run 2b. Water Quality Classification of nearest receiving water: See Form WSCAS, and Map of Stream Crossings which are attached 2c. River basin: map is available at http://h2o,enr.state.nc.us/admin/maps/ Neuse, See Map 3. Project Description 3a. Describe the existing conditions on the site and the general land use in the vicinity of the project at the time of this application: A 30 inch sewer outfall extends East along Briery Run Stream from Airport Road to Wallace Family Road The adjacent land is presently Zoned RA -6 RA -20 and RA -12 The Sewer line runs along the edge of the 100 year Flood plain and occasionally dips into the flood plain and crosses the flood plain of Briery Run The surrounding area for the most part is cultivated farm land The sewer line and the cleared easement is within Bottom land Forest/Hardwood Swamps9 and other Broadleaf Deciduous Forest which are associated with wetlands on the Land Cover Map The Sewer line is shown to run adjacent to and cross the wetlands associated with Briery Run on the Project Access Map. 3b. List the total estimated acreage of all existing wetlands on the property: 155.88 See attached Table: "Property and Easement Information" and Project Access Map, 3c. List the total estimated linear feet of all existing streams (intermittent and perennial) on the property: 24,745 feet See attached Table: "Property and Easement Information" and Stream Crossing Map 3d. Explain the purpose of the proposed project: The 30 inch concrete sewer was installed in the early 1970s and has developed leaks and is experiencing deterioration due to hydrogen sulfide The ipe is structurally sound but the manholes have developed leaks and need to be rehabilitated The City plans to rehabilitate the line and manholes using a no dig, CIPP method Temporary access using construction mats is being proposed so that the impact to the wetlands will be minimal. 3e. Describe the overall project in detail, including the type of equipment to be used: The rehabilitation of the Briery Run Sewer line has been a multi -phase project The proposed Phase IV will consist of providing access to the 14,824 feet of sewer line using construction mats, 39 of the 49 manholes will be raised a cured in place rehabilitation of 36 of the 49 manholes and a cured in place rehabilitation of 4,290+/- feet of the 30 inch sewer line. A Sewer System Evaluation Survey was performed and an Engineering Report and Environmental Impact Document were completed to determine the scope of the project The final Phase Phase V of the rehabilitation will be a future project once funding has been established See the attached Erosion Control Project Description with the Erosion Control Permit Application, for more details. Page 3 of 12 PCN Form —Version 1.3 December 10, 2008 Version 4. Jurisdictional Determinations 4a. Have jurisdictional wetland or stream determinations by the Corps or State been requested or obtained for this property / project (including all prior phases) in the past? Comments: Areas taken from NC GIS, and NC Land Use Maps.. See attached Wetland Narrative. X Yes ❑ No ❑ Unknown 4b. If the Corps made the jurisdictional determination, what type of determination was made? X Preliminary ❑ Final 4c. If yes, who delineated the jurisdictional areas? Name (if known): See attached Wetland Narrative Agency/Consultant Company: Other: 4d. If yes, list the dates of the Corps jurisdictional determinations or State determinations and attach documentation. Determinations were made by both the Corps and the State on July 11, 2017. See attached letter 5. Project History 5a. Have permits or certifications been requested or obtained for this project (including all prior phases) in the past? ❑ Yes ❑ No X Unknown 5b. If yes, explain in detail according to "help file" instructions. N/A 6, Future Project Plans 6a. Is this a phased project? X Yes ❑ No 6b. If yes, explain. This project is Phase IV of a project which has been ongoing for 15 years Rehabilitation of Briery Run Sewer. Before the project was begun The Waste water treatment plant would experience influent flows in excess of the permitted limit during heavy rainfall events Phase I was completed in 2001, and included rehabilitation of 14 manholes and 2,482 feet of 30 inch Sewer line between Highway I I and the Briery Run Liftstation Phase II of the rehabilitation included 1,333 feet of 15" sewer and 435 feet of 24" sewer and replacement of 12 manholes between Rouse Road and Graham Drive and was completed in 2006. Phase III of the rehabilitation included 1 137 feet of 30 inch sewer line and replacement of 12 manholes between Graham Drive and Airport Road and was completed in 2010 Phase IV will rehabilitate Raise 39 manholes rehabilitate 36 manholes and rehabilitate 4,290 feet of 30" Sewer line between Airport Road and Wallace Family Road A future Phase V Rehabilitation is planned for the Sewer line between Wallace Family Road and Highway 11 After Phase V is completed The City will evaluate past phases to fill in gaps left due to the lack of funds because each Phase was limited because of the funds available for the project The City plans to complete Phase V in 2019 to 2020 pending approval of the funding and permitting. Page 4 of 12 C. Proposed Impacts Inventory 1. Impacts Summary 1a. Which sections were completed below for your project (check all that apply): X Wetlands X Streams - tributaries X Buffers ❑ Open Waters ❑ Pond Construction 2. Wetland Impacts If there are wetland impacts proposed on the site, then complete this question for each wetland area impacted. 2a. 2b, 2c. 2d, 2e. 2f. Wetland impact Type of jurisdiction number — Type of impact Type of wetland Forested* (Corps - 404, 10 Area of impact Permanent (P) or (if known) DWQ — non -404, other) (acres) Temporary T W1 ❑ P XT Temporary Access Riverine Swamp ❑ Yes X Corps 0.15 Crossing Forrest X No X DWQ W2 ❑ P XT Temporary Access Bottomland ❑ Yes X Corps 0.36 Crossing Hardwood X No X DWQ W3 ❑ P X T Temporary Access Bottomland ❑ Yes X Corps 0.22 Crossing Hardwood X No X DWQ W4 ❑ P X T Temporary Access Bottomland ❑ Yes X Corps 0.02 Crossing Hardwood X No X DWQ ❑ P X T Temporary Access Bottomland ❑ Yes X Corps 0.11 W5 Crossing Hardwood X No X DWQ W6 ❑ P X T Temporary Access Riverine Swamp ❑ Yes X Corps 0.72 Crossing Forrest X No X DWQ W7 ❑ P X T TemporaryAccess Riverine Swamp ❑ Yes X Corps 0.12 Crossing Forrest X No X DWQ 2g. Total wetland impacts 1.70 2h. Comments:*Forested around cleared easement. See Project Access Map. Although more than 1 acre is impacted, the Impact is necessary, temporary (Construction Mats) and minimized. See Section D 1 1a and b on page 7 of 12. 3. Stream Impacts If there are perennial or intermittent stream impacts (including temporary impacts) proposed on the site, then complete this question for ail stream sites impacted. *Water ponding at the crossing, Temporary Crossing with Construction Mats. 3a. 3b, 3c, 3d. 3e. 3f. 3g. Stream impact Type of impact Stream name Perennial Type of jurisdiction Average Impact number - (PER) or (Corps - 404, 10 stream length Permanent (P) or intermittent DWQ — non -404, width (linear Temporary (T) (INT)? other) (feet) feet) S1 EJ P X T Temporary UT to Briery Run* X PER X Corps 40 10 Crossing ❑ INT X DWQ S2 F1 P X T Temporary Briery Run X PER X Corps 10 10 Crossing ❑ INT X DWQ S3 F-1 P X T TC Brieemprary ry Run X PER X Cs 15 10 ossi g ❑ NT X DWQ S4 ❑ P X T Temporary Briery Run X PER X Corps 15 10 Crossing ❑ INT X DWQ S5 ❑ P X T Temporary Briery Run X PER X Corps 15 10 Crossing ❑ INT X DWQ S6 ❑ P X T Temporary UT to Briery Run X PER X Corps 5 10 Crossing ❑ INT I X DWQ S7 ❑ P X T Temporary UT to Briery Run El PER X Corps 40 10 Crossing X INT X DWQ 3h. Total stream and tributary impacts 70 Page 5 of 12 3i. Comments: Of the 7 stream crossings 4 crossings are for briery Run, and 3 are unnamed tributaries to Briery Run See the Stream Crossing Map, 4. Open Water Impacts If there are proposed impacts to lakes, ponds, estuaries, tributaries, sounds, the Atlantic Ocean, or any other open water of the U.S. then indii idually list all open water impacts below. 4a. Open water impact number — Permanent (P) or Temporary T 4b. Name of waterbody (if applicable) 4c. Type of impact 4d. Waterbody type 4e. Area of impact (acres) 01 ❑ P ❑ T N/A N/A N/A N/A 02 ❑ P ❑ T N/A N/A N/A N/A 03 ❑ P ❑ T N/A N/A N/A N/A 04 ❑ P ❑ T N/A N/A N/A N/A 4f. Total open water impacts N/A 4g. Comments: N/A 5. Pond or Lake Construction If pond or lake construction proposed, then complete the chart below. 5a. Pond ID number 5b, Proposed use or purpose of pond 5c. Wetland Impacts (acres) 5d. Stream Impacts (feet) 5e. Upland (acres) Flooded Filled Excavated Flooded Filled Excavated Flooded P1 N/A N/A N/A N/A N/A N/A N/A N/A P2 N/A N/A N/A N/A N/A N/A N/A N/A 5f. Total N/A N/A N/A N/A N/A N/A N/A 5g. Comments: N/A 5h. Is a dam high hazard permit required? ❑ Yes X No If yes, permit ID no: 5i. Expected pond surface area (acres): N/A 5j. Size of pond watershed (acres): N/A 5k. Method of construction: N/A Page 6 of 12 6. Buffer Impacts (for DWQ) If project will impact a protected riparian buffer, then complete the chart below. If yes, then individually list all buffer impacts below. If any impacts require mitigation, then you MUST fill out Section D of this form. 6a. X Neuse ❑ Tar -Pamlico ❑ Other: Project is in which protected basin? ❑ Catawba ❑ Randleman 6b. 6c, 6d, 6e, 6f. 6g. Buffer impact number — Reason Buffer Zone 1 impact Zone 2 impact Permanent (P) for impact Stream name mitigation (square feet) (square feet) or Temporary required? T B1 ❑ P XT Temporary Crossing UT to Briery Run EI Yes X No 600 400 B2 El P X T Temporary Crossing Briery Run ❑X Yes 600 400 B3 ❑ P X T Temporary Crossing Briery Run El Yes X No 600 400 B4 ❑ P X T Temporary Crossing Briery Run El Yes X No 600 400 B5 ❑ P X T Temporary Crossing Briery Run ❑ Yes X No 600 400 B6 ❑ P X T Temporary Crossing UT to Briery Run ❑ Yes X No 600 400 B7 ❑ P XT Temporary Coss UT to Briery Run EI YNo 600 400 6h. Total buffer Impacts 41200 2,800 61. Comments: The Buffer is In an area that is maintained for the Sewer line maintenance in accordance with the Neuse Buffer Rules and because the sewer line and the cleared buffer existed in 1973, prior to July 22, 1997, in accordance with 15 NCAC 02B .0233 (3) (b) (i). Any additional impacts to the Buffers will be temporary. Buffer will be reestablished as it was before the project when project is complete. Impacts to stream crossings, riparian buffers and wetlands will be temporary and minimized by using construction mats, and any Impacts will be repaired once the project is over. D. Impact Justification and Mitigation 1. Avoidance and Minimization 1a. Specifically describe measures taken to avoid or minimize the proposed impacts in designing project. By using construction mats to provide access for the construction equipment, impacts to wetlands, streams and riparian buffers will be minimized for this project. By using Trenchless techniques in the rehabilitation the impacts to the wetlands, streams and riparian buffers will be minimized. Part of the construction effort involves reestablishing vegetation so any temporary impacts will mitigated. b. Specifically describe measures taken to avoid or minimize the proposed impacts through construction techniques. The project will use trenchless technology for the rehabilitation where ever it is possible. Manholes and pipe will be rehabilitated using cured in place methods wherever it is possible. Construction mats will be used for access, and the construction mats will be removed as soon as possible. A vegetative cover will be established prior to close out of the project. Page 7 of 12 2. Compensatory Mitigation for Impacts to Waters of the U.S. or Waters of the State 2a. Does the project require Compensatory Mitigation for ❑ Yes X No Type N/A impacts to Waters of the U.S. or Waters of the State? 3c, Comments: N/A 4. 2b. If yes, mitigation is required by (check all that apply): 4a. ❑ DWQ ❑ Corps 4b. Stream mitigation requested: ❑ Mitigation bank 2c. If yes, which mitigation option will be used for this project? 4d. ❑ Payment to in -lieu fee program square feet 4e. Riparian wetland mitigation requested: ❑ Permittee Responsible Mitigation 3. Complete if Using a Mitigation Bank N/A 3a. Name of Mitigation Bank: N/A 3b, Credits Purchased (attach receipt and letter) Type N/A Quantity N/A 3c, Comments: N/A 4. Complete if Making a Payment to In -lieu Fee Program N/A 4a. Approval letter from in -lieu fee program is attached. ❑ Yes 4b. Stream mitigation requested: linear feet 4c. If using stream mitigation, stream temperature: ❑ warm ❑ cool ❑cold 4d. Buffer mitigation requested (DWQ only): square feet 4e. Riparian wetland mitigation requested: acres 4f. Non -riparian wetland mitigation requested: acres 4g. Coastal (tidal) wetland mitigation requested: acres 4h. Comments: NIA S. Complete if Using a Permittee Responsible Mitigation Plan 5a. If using a permittee responsible mitigation plan, provide a description of the proposed mitigation plan. The permittee plans to require installation of construction mats for temporary access and no changes will be made to the flow characteristics of the runoff. Once vegetation is re-established, there will be no evidence that the project took place. Page 8 of 12 6. Buffer Mitigation (State Regulated Riparian Buffer Rules) —required by DWQ 6a. Will the project result in an impact within a protected riparian buffer that requires F1 Yes X No buffer mitigation? If Yes you will have to fill out this entire form — please contact the State for more information. 6b. If yes, then identify the square feet of impact to each zone of the riparian buffer that requires mitigation. Calculate the amount of mitigation required. 6c. 6d. 6e. Reason for impact Total impact Multiplier Required mitigation Zone (square feet) (square feet) Zone 1 3 (2 for Catawba) Zone 2 1.5 6f. Total buffer mitigation required: 6g. If buffer mitigation is required, discuss what type of mitigation is proposed (e.g., payment to private mitigation bank, permittee responsible riparian buffer restoration, payment into an approved in -lieu fee fund). N/A 6h, Comments: After the construction project is completed, the Buffer Areas will be returned to the pre -construction condition. Page 9 of 12 E. Stormwater Management and Diffuse Flow Plan (required by DWQ) 1. Diffuse Flow Plan 1a. Does the project include or is it adjacent to protected riparian buffers identified X Yes ❑ No within one of the NC Riparian Buffer Protection Rules? 1 b. If yes, then is a diffuse flow plan included? If no, explain why. Comments: Stormwater routing and flow characteristics will not be change by F-1 Yes X No the construction project. Diffuse flow will be maintained, and flow will be overland, and every attempt will be made to reduce point source flows into collector tributaries. 2. Stormwater Management Plan 2a. What is the overall percent imperviousness of this project? 0.00% 2b. Does this project require a Stormwater Management Plan? ❑ Yes X No 2c. If this project DOES NOT require a Stormwater Management Plan, explain why: The project will not change the flow characteristics of the stormwater runoff. Silt, Sediment and Erosion Control Plan insures the water quality of the runoff, and the project will comply with the previously approved Kinston Stormwater Management Plan for Nitrogen Control. 2d. If this project DOES require a Stormwater Management Plan, then provide a brief, narrative description of the plan: N/A 3. Certified Local Government Stormwater Review 3a. In which local government's jurisdiction is this project? The City of Kinston has Kinston, North Carolina set up a Stormwater Utility to implement and enforce the Neuse Rules ❑ Phase II X NSW 3b. Which of the following locally-implemented stormwater management programs ❑ USMP apply (check all that apply): ❑ Water Supply Watershed ❑ Other: 3c. Has the approved Stormwater Management Plan with proof of approval been ❑ Yes X No attached? 4. DWQ Stormwater Program Review ❑ Coastal counties ❑ HOW 4a. Which of the following state-implemented stormwater management programs apply ❑ ORW (check all that apply): ❑ Session Law 2006-246 X Other: Neuse Rules 4b. Has the approved Stormwater Management Plan with proof of approval been ❑ Yes X No attached? 5, DWQ 401 Unit Stormwater Review 5a. Does the Stormwater Management Plan meet the appropriate requirements? X Yes ❑ No 5b. Have all of the 401 Unit submittal requirements been met? X Yes ❑ No Page 10 of 12 PCN Form —Version 1.3 December 10, 2008 Version F. Supplementary Information 1, Environmental Documentation (DWQ Requirement) la. Does the project involve an expenditure of public (federal/state/local) funds or the X Yes ❑ No use of public (federal/state) land? 1b. If you answered "yes" to the above, does the project require preparation of an environmental document pursuant to the requirements of the National or State X Yes ❑ No (North Carolina) Environmental Policy Act (NEPA/SEPA)? 1c. If you answered "yes" to the above, has the document review been finalized by the State Clearing House? (If so, attach a copy of the NEPA or SEPA final approval letter.) X Yes ❑ No Comments: Categorical Exclusion Letter is Attached. See Letter Dated November 1, 2016, from Seth Robertson, PE, Chief State Revolving Fund Section. 2. Violations (DWQ Requirement) 2a. Is the site in violation of DWQ Wetland Rules (15A NCAC 2H .0500), Isolated Wetland Rules (15A NCAC 2H .1300), DWQ Surface Water or Wetland Standards, ❑ Yes X No or Riparian Buffer Rules (15A NCAC 2B.0200)? 2b. Is this an after -the -fact permit application? ❑ Yes X No 2c. If you answered "yes" to one or both of the above questions, provide an explanation of the violation(s): NIA 3, Cumulative Impacts (DWQ Requirement) 3a. Will this project (based on past and reasonably anticipated future impacts) result in X Yes ❑ No additional development, which could impact nearby downstream water quality? 3b. If you answered "yes" to the above, submit a qualitative or quantitative cumulative impact analysis in accordance with the most recent DWQ policy. If you answered "no," provide a short narrative description. The project will rehabilitate the existing sewer which and not an expansion of the sewer collection system, but the improved efficiency of the existing sewer line will and allow for increased flow and increased permitted flow. However, no more flow will be allowed than was included in the original plan when the line was permitted. 4. Sewage Disposal (DWQ Requirement) 4a. Clearly detail the ultimate treatment methods and disposition (non -discharge or discharge) of wastewater generated from the proposed project, or available capacity of the subject facility. Sewage from the development will ultimately be treated by the Kinston Water Reclamation Facility which presently treats an Average Daily Flow of 4.56 MGD and the design capacity is 11.85 MGD. The Treatment Plant uses the Johannesburg Process which provides tertiary treatment for nitrogen removal and denitrification filters are also part of the treatment process by providing additional denitrification and effluent polishing by filtration Disinfection is provided by Ultra Violet light. Page 11 of 12 So Endangered Species and Designated Critical Habitat (Corps Requirement) 5a. Will this project occur in or near an area with federally protected species or ❑ Yes X No habitat? 5b. Have you checked with the USFWS concerning Endangered Species Act X Yes ❑ No impacts? X Raleigh 5c. If yes, indicate the USFWS Field Office you have contacted. ❑ Asheville 5d. What data sources did you use to determine whether your site would impact Endangered Species or Designated Critical Habitat? For the Engineering Report and Environmental Impact Document, I used the United States Fish and Wildlife web site, www.fws.gov, 6. Essential Fish Habitat (Corps Requirement) 6a. Will this project occur in or near an area designated as essential fish habitat? ❑ Yes X No 6b. What data sources did you use to determine whether your site would impact Essential Fish Habitat? For the Engineering Report and Environmental Impact Document, I used the United States Fish and Wildlife website, www.fws.aov. 7. Historic or Prehistoric Cultural Resources (Corps Requirement) 7a. Will this project occur in or near an area that the state, federal or tribal governments have designated as having historic or cultural preservation ❑ Yes X No status (e.g., National Historic Trust designation or properties significant in North Carolina history and archaeology)? 7b. What data sources did you use to determine whether your site would impact historic or archeological resources? For the Engineering Report and Environmental Impact Document, I used the North Carolina Natural Heritage web site, www.ncnhp.org. 6. Flood Zone Designation (Corps Requirement) Be, Will this project occur in a FEMA -designated 100 -year floodplain? X Yes ❑ No 8b. If yes, explain how project meets FEMA requirements: As part of this Project the top of all Manholes will be raised to two feet above the 100 year Flood elevation. 8c. What source(s) did you use to make the floodplain determination? FIRM Maps and GIS Mapping 1lican rZ2/1Zl% Tony Sears, City Manager Ply Applicant/Agent's Printed Name Date A Agent's Signature (Agent's signature is valid only if an authorization letter from the applicant Isprovided.) Page 12 of 12 Version 1.4 January 9, 2009 401 & Buffer Permitting PCN Submittal Checklist X The application fee (Checks may be made out to "N.C. Division of Water Resources" $240.00 for 401 Water Quality Certification with minor impacts $570.00 for 401 Water Quality Certification with major impacts Express Review Fee (Amount requested on Acceptance Letter) X Four (4) complete and collated copies of the PCN Application and supporting documentation (instead of providing 4 copies of the full size plans you may provide two copies of full size plans along with two copies of 11 X 17 plans) X Stormwater Management Plan (if applicable — see PCN Form Help File Section E) I. No Changes in Stormwater Routing or overland flow, and no changes in impervious area. 1) Please provide three (3) copies of the stormwater management plans along with all supporting information pertaining to this project including the following: a. Entire site development/layout plans delineating all drainage areas; b. Design calculation sheets for all proposed BMP(s) sized for both on-site and off-site drainage; c. BMP supplements for each proposed BMP and Required Items Check List (htti)://portal ncdenr org/web/Ir/bmp-manual) along with all required items; d. A Notarized Operation & Maintenance Agreement for each stormwater management facility; e. Detailed construction drawing sheets shall include (i) Erosion and sediment control plans; (ii) Installation and planting schedules for the proposed BMPs; (iii) Appropriately scaled plan views and cross sectional details of all BMPs and associated components — inlet and outlet structures, forebay, respective zones and pertinent elevations. X If your project is located within a State implemented Riparian Buffer Rule Area, submit the following along with site plans and PCN form: 1) Three (3) copies of the details for on-site diffuse flow provisions, (refer to http://portal.ncdenr.org/web/Ir/bmp-manual . X DWR Stream Determination Forms for streams on property and DWR determination letter for wetlands or streams (if applicable). The following is the most critical of all the information that you must provide. The quality and detail of the information will often determine the expeditiousness of the review. The following is a checklist of the types of pertinent information required at a minimum: Maps and Plans: X The most recent version of the 1:24,000 USGS Topographic Map - Please cleanly draw or delineate the site boundaries on the topographic map. X The most recent version of the bound and published County NRCS Soil Survey Map - (required for projects within the Neuse River Basin, Tar -Pamlico River Basin, Randleman Lake Watershed and the Catawba River Basin, also recommended for all projects) - Please clearly delineate the site boundaries, etc. on the map. If the delineation obscures Version 1.4 January 9, 2009 any of the features, it is recommended that a clean copy be provided. Copies of the current soil survey and/or soil survey map sheets can be obtained from the local NRCS County Office (hftp://www.nc.nrcs.gLda.govn. GIS soil layers are not acceptable. X Vicinity map - Please clearly mark the location and approximate boundaries of the property and project on the map. Please indicate north arrow and scale. Please include applicable road names or State Road numbers. X The Site Plan - The most critical map to be provided is the site plan. You must provide full sized plans. The following is the minimum list of plans that are typically needed. X Pre-construction/Pre-existing conditions -This sheet (or sheets) must include: • All jurisdictional and non -jurisdictional wetland, stream, water features, State regulated buffers (delineated into Zones 1 and 2) Topographic contours with elevations Any existing structures and impervious areas • Existing utility lines and easements Existing roads, culverts, and other pertinent features North arrow and the scale (1":50' scale is recommended). X Proposed conditions -This sheet (or sheets) must include: • All jurisdictional and non -jurisdictional wetland, stream, water features, State regulated buffers (delineated into Zones 1 and 2) Lot layout (if a subdivision or commercial development is proposed) - lots must be developable without further impacts to jurisdictional and non -jurisdictional wetlands, streams water features and State regulated buffers. Building envelopes must be provided when streams, wetlands, riparian buffers, or water features exist on a lot • All built -out structures and impervious cover • Final grading contours with elevations • All utilities and easements (including septic fields on all lots within 100 feet of stream, wetland, or water features - if applicable) • Impacted areas — these should correspond with the Impact numbers listed on your PCN form. X Drainage Plans -Final drainage plans must include the following: • Locations and pertinent elevations and sizes of the stormwater collection system and drainage ways All inlets and outlets must also be shown with pertinent elevations (All outlets to wetlands must be at a non-erosive velocity, generally less than 2 ft/sec during the peak flow from the 10 -yr storm) • Scaled stormwater BMPs must also be indicated as required by DWR rules and policies In certain cases (see Section E of PCN form), final stormwater management plans must also be provided (see Stormwater Management Plan Checklist) X Proposed Impacts -All impacts to jurisdictional and non -jurisdictional wetland, stream, water features, and State regulated buffers must be shown and labeled on the site plans at a scale no smaller than 1" = 50'. All excavation, fill, flooding, stabilization, and other impacts that will be conducted in or near jurisdictional and non -jurisdictional wetland, stream, water features, and State regulated buffers must be indicated. Please provide cross sectional Version 1.4 January 9, 2009 details showing the provisions for aquatic life passage (burial of culvert 20% for culverts 5 48 inches, and 1 -foot for culverts > 48 inches). Wetland Impacts: SEE NARRATIVE X Precise grading and final elevation contours must be provided. Existing vegetation and any clearing must be specified. X All subsurface utility lines must indicate the location of anti -seep collars. Construction detail for anti -seep collars must be provided. X Roadway or other crossings of riparian wetlands may require floodway culverts to maintain existing hydrological conditions. X Plans should show that the hydrology of remaining wetlands on the site will be maintained. Stream Impacts: X Stream impacts must be clearly shown on the plans. The centerline as well as the banks of the stream must be surveyed or located by GPS for the portion of the stream to be impacted. N/A The inlet and the outlet of all culverts should be aligned with the stream as much as possible. Inlet and outlet elevations and streambed elevations should be indicated. Any inlet or outlet protection must be shown and enumerated on the impact map(s). NIA For bottomless culverts or other spans, a vertical cross section should be provided that shows the minimum distance from each span to each stream bank, the stream cross section, the height of the span above the stream and the minimum distance from the edge of each footer to each stream bank. Additionally, please provide a signed and sealed geotechnical report of subsurface soils at the proposed bottomless culvert location. The report must comply with the Division of Highways — Guidelines for Drainage Studies and Hydraulic Design, prepared by A.L. Hankins, Jr., State Hydraulics Engineer - 1999. N/A Multiple culverts or sectioned box culverts typically require the use of sills, off - setting or other means to match the cross section of the existing stream (in order to maintain stream stability and provide aquatic life passage). A vertical cross section of the culverts should be shown overlain with the up and downstream stream cross section including the stream flood -prone area. N/A Impacts associated with dam construction must indicate and enumerate all fill associated with the dam footprint, spillway and any bank stream bank stabilization. The length of stream impounded must also be indicated and enumerated. § ! § B 5 E § [ { ] ! E } Cd 2f k\ \ \ \ \ \ \ \ \ \ \ \ \ \ \ \ \ \ \ ( ;§ ;( !) !§ 0m w( !m \ !§ § !2 !2 r: §2 J: Z2 22 22 l2 }{ ){ U0 {§f ~ { /f 27 ;f ]) ®: 3 z \ : - - - § . )) \) ]) E E) 0 00 !2{ /® §)2 2R «( ®f {} j2 !& )2 !{ - !2 3; !J «{ «/ ){ )\ /\ to; (() j{ §) \) §) §) §7 §i \) \\ §\ §\ §k !) N) :7 -- - (} ) - - _ \( :/)] f) �\ !F Q _ § §k ! �! :aK ,! «, !: !: ,!!!§!§& ; z/ 6 \ \ \ \ \ \ \ \ \ \ \ \ \ � City of Kinston Phase IV Briery Run Sewer Rehabilitation 3/27/17 t p l The project is located along Briery Run, one of the streams which collects runoff from the Kinston/ Lenoir County area and flows to Stoneyton Creek and on to the Neuse River. The rehabilitation of the Sewer line which follows this stream has been a multi phased project. Phase I, II, and III have been completed. The current project is Phase IV of the Briery Run Sewer Rehabilitation and is for the rehabilitation of the Briery Run Sewer from Airport Road to Wallace Family Road. The line is a thirty (30) inch Sewer Outfall, and it is being rehabilitated because of the deterioration which has occurred, and the extreme amount of Inflow and Infiltration which is occurring. In order to minimize erosion the rehabilitation will use a no dig solution. However, access will be difficult, so construction mats are proposed to protect the wetlands and to reduce and control the land disturbing activities on this project. Any future maintenance activities on this section of the Sewer line will also use construction mats. In Phase IV of the Briery Run Sewer Rehabilitation, thirty nine (39) manholes will be raised, then thirty- six (36) manholes will be rehabilitated using a cured in place liner.in the manhole. This is a no dig solution, so the only land disturbance will be the access. In addition the project will include rehabilitation of 4,238 feet of 30 inch concrete pipe with a cured in place liner. The rehabilitation method is also a no dig solution, so the only land disturbance will be the access to the site. The construction sequence will be: 1. The First Step will be the installation of the silt fence on the down gradient side of the access path, and / or between the proposed path and Briery Run Creek. 2. The Second Step will be to install the creek crossings which are a combination of two rock check dam with a rock lined bottom across the creels. 3. The Third Step in the construction process will be laying out the 14,824 feet of access construction mats on the path which has already been cleared and is maintained as required by DWQ. This layout will cause minor disturbance of 3.4 acres as proposed in the FINANCIAL RESPONSIBILITY/OWNERSHIP FORM SEDIMENTATION POLUTION CONTROL ACT. 4. The Fourth Step will be to raise the thirty-nine (39) manholes that are less than 2 feet above the 100 year Flood elevation. 5. The Fifth Step will be the rehabilitation of the thirty-six (36) manholes using a cured in place rehabilitation method. 6. The Sixth Step will be the rehabilitation of the sections of the sewer pipe which have been prioritized the rehabilitation will use a cured in place method. 7. The Seventh Step will be revegetation of the land which will have been disturbed including the area where the construction mats will have been placed. Once vegetation has been established, the vegetation will naturally prevent erosion, and City of Kinston Phase IV Briery Run Sewer Rehabilitation 3/27/17 sediment will be deposited from the runoff which will be slowed by the vegetation. 8. Finally, the Eighth Step once the vegetation is established, the silt fences will be removed. STREAM CROSSING NARRATIVE The Form WSCAS; which lists the location, Name of the stream, County, River Basin, Stream Index Number and the Stream Classification for each stream which was crossed; was completed; and it is attached. As part of the Form WSCAS, an 8.5 X 11 USGS map of the project area is attached. In addition an evaluation was done by Anthony Scarbraugh and Chris Pullinger of the Division of Water Resources in the field on July 11, 2017, and it was documented by a letter from Robert Tankard dated July 26, 2017. The letter included five stream evaluations, and the field notes on a USDA Lenoir County Soils Map, and a USGS Map. The Letter and attachments are included. The Determination was that Briery Run and two of the streams that were crossed were subject to the Neuse buffer rules. From the Briery Run Phase IV Stream Crossing Map, Stream Crossing number 7 was not considered subject to the Neuse Buffer Rules. Stream Crossing number 1, from Station 110+98.2 to Station 111+29.1, consists of a large ponding area over the sewer line, but the stream flows into the ponding area and out of the ponding area and into Briery Run. The stream is an unnamed tributary to Briery Run, and the stream drains overflow from a pond which is up hill from Briery Run A picture of the crossing is on the bottom of page 3. This crossing is subject to the Neuse Buffer Rules, but the stream bank is not well defined, and any flow of stormwater will be overland to the ponding area. It is anticipated that a construction mat will be used for the construction equipment crossing this stream. No other modifications will be constructed for access. The top of the Stream Bank is well defined so the edge of water was used as top of Bank, and the Buffers are delineated as Zone 1 from Station 110+68.2 to Station 110+98.2, and from Station 111+29.1 to Station 111+59.1. Zone 2 is delineated from Station 110+48.3 to Station 110+68.2, and from Station 111+59.1 to Station 111+79.1. See Plan Sheet 9 Of 14, Stream Crossing number 2, from Station 68+91.7 to Station 69+11.8, is just east of Highway 58 North. This stream crossing is a crossing of Briery run, and it is subject to the Neuse Buffer Rules. The channel and stream bank at this crossing are well defined, but the Northern bank is approximately 3 feet higher than the Southern bank. The Northern bank will have to be graded so that construction equipment can cross the stream at this point. Once the bank is graded, equipment will use a construction mat for the crossing. Once construction is finished, the stream bank will be revegetated. There is a picture of this stream crossing on the top of page 4. The Banks are well defined. No other modifications will be constructed for access. Since the tops of the Stream Banks are well defined, the Buffers are delineated as Zone 1 from Station 68+61.7 to Station 68+91.7, and from Station 69+11.8 to Station 69+43.6, Zone 2 is delineated from Station 68+41.7 to Station 68+61.7, and from Station 69+43.6 to Station 69+70.4, See Plan Sheet 6 of 14. Stream Crossing number 3, from Station 65+87.8 to Station 65+97.8, is a crossing of Briery Run, and it is subject to the Neuse Buffer Rules. The Channel and the stream bank are well defined and neither approach to the crossing is too steep. It is anticipated that equipment will use a construction mat for the crossing. There should be no adverse effect of the construction equipment crossing the stream crossing at this location. There is a picture of the stream crossing on the bottom of page 4. The Banks are well defined. No other modifications will be constructed for access. Since the tops of the Stream Banks are well defined, the Buffers were delineated as Zone 1 from Station 65+57.8 to Station 65+87.8, and from Station 65+97.8 to Station 66+27.8. Zone 2 is delineated from Station 65+37.8 to Station 65+57.8, and from Station 66+27.8 to Station 66+47.8, See Plan Sheet 6 Of 14, Stream Crossing number 4, from Station 64+27.8 to Station 64+38.2, is a crossing of Briery Run, and it is subject to the Neuse Buffer Rules, The Channel and the stream bank are well defined and neither approach to the crossing is too steep. It is anticipated that equipment will use a construction mat for the crossing. There should be no adverse effect of the construction equipment crossing the stream crossing at this location. There is a picture of the stream crossing on the top of page 5. The Banks are well defined. No other modifications will be constructed for access. Since the tops of the Stream Banks are well defined, the Buffers are delineated as Zone 1 from Station 63+96.7 to Station 64+27.8, and from Station 64+38.2 to Station 64+69.3. Zone 2 is delineated from Station 63+75.9 to Station 63+96.7, and from Station 64+69.3 to Station 64+90.1. See Plan Sheet 6 of 14. Stream crossing Number 5, from Station 59+07.2 to Station 59+29.9, is a crossing of Briery Run, and it is subject to the Neuse Buffer Rules. The Channel and the stream bank are well defined and neither approach to the crossing is too steep. It is anticipated that equipment will use a construction mat for the crossing. There should be no adverse effect of the construction equipment crossing the stream crossing at this location. There is a picture of the stream crossing on the bottom of page 5. This crossing is subject to the Neuse Buffer Rules. No other modifications will be constructed for access. Since the tops of the Stream Banks ar well defined, the Buffers are delineated as Zone 1 from Station 58+61.9 to Station 59+07.2, and from Station 59+29.9 to Station 59+75.2, Zone 2 is delineated from Station 58+31.7 to Station 58+61.9, and from Station 59+75.2 to Station 60+05.4. See Plan Sheet 6 of 14. Stream Crossing number 6, from Station 54+9 0.3 to Station 55+05.5, is a crossing of an unknown tributary to Briery Run, and it is subject to the Neuse Buffer rules. The picture of the crossing at the top of page 6 shows a Stream with very little water flowing, the picture was taken in the summer after a prolonged dry spell. The stream flows from the stormwater pond in the Briery Subdivision. The channel and the banks are well defined. The stream is an intermittent stream. The Banks are low with little slopes to the channel. The construction equipment will use a construction mat to make the crossing. This crossing is subject to the Neuse Buffer Rules, and the Banks are well defined. No other modifications will be constructed for access. Since the tops of the Stream Banks are well defined, the Buffers are delineated as Zone 1 from Station 54+60.3 to Station 54+90.3, and from Station 55+06.5 to Station 55+35.5. Zone 2 is delineated from Station 54+40.3 to Station 54+90.3, and from Station 55+35.5 to Station 55+55.5, See Plan Sheet 5 of 14. Stream Crossing number 7, from Station 30+15.9 to Station 30+25.9, is an unnamed tributary to Briery Run, and according to the field determination by Water Resources on July 11, 2017, it is not subject to the Neuse Buffer Rules. The evaluation that I made in the field on September 26, 2017, is based on the picture on the bottom of page 6, which shows a stream flowing across the sewer line right of way. The channel is well defined, but the low banks make it difficult to define the Top of Bank. The stream drains from an upland pond, and an upland field. In addition the wetlands, which are over the sewer line right of way to the Easl, slowly flows overland to this stream. I believe that this stream although it may be intermittent, it should be subject to the Neuse Buffer Rules. Construction equipment will use a construction mat to cross the stream at this location, and there should be no adverse effects of the construction. This crossing is subject to the Neuse Buffer Rules, and the Banks are well defined. No other modifications will be constructed for access. Since the tops of the Stream Banks are well defined, the Buffers are delineated as Zone 1 from Station 29+85.9 to Station 30+15.9, and from Station 30+25.9 to Station 30+55.9, Zone 2 is delineated from Station 29+65.9 to Station 29+85.9, and from Station 30+55.9 to Station 30+75.9. See Plan Sheet 4 of 14. Stream Crossing #1 stream flows through localized pond to Briery Run � °« :33:\'w» pj®/\ . kramc _sng3e���� E Ii eylop ff°rd ;I Stream Crossing 4 Briery Run Stream Crossing 5 Briery Run OPT,_ . t. K r _I �' r ji Stream Crossing 6 Unnamed Tributary to Briery Run from Briery Pond Stream Crossing 7 Unnamed Tributary to Briery Run from Pond and Wetlands 2 OF W ATFR FORM WSCAS�03/2012 0 OG WATERSHED CLASSIFICATION ATTACHMENT o � FOR SEWER SYSTEMS Applicant Name Proiect Name City of Kinston Phase IV Briery Run Sewer Rehabilitation Professional Engineer Name Engineering Firm Name John A. Jarrell, III, P.E. City of Kinston Engineering Division Location t If unnamed, indicate "unnamed tributary to X", where X is the named waferbody to which the unnamed tributary River Waterbody Stream Waterbody ID Name of Waterbod ' County Basin Index No. Classification Lat. 35.312711 Unnamed Tributary to Briery Lenoir Neuse 27-81-1- C,NSW Long, Run 77.563996 Lat. 35.309722 Briery Run Lenoir Neuse 27-81-1 C,NSW Long. 77.563853 Lat. 35.507574 Briery Run Lenoir Neuse 27-81-1 C,NSW Long. 77.563853 Lat. 35:308251 Briery Run Lenoir Neuse 27-81-1 C,NSW Long, 77.563967 Lat, 35.31466 Briery Run Lenoir Neuse 27-81-1 C,NSW Long, 77.554783 Lat. 35.313983 Unnamed Tributary to Briery Lenoir Neuse 27-81-1- C,NSW Long. Run 77.554884 Lat. 35.31529 Unnamed Tributary to Briery Lenoir Neuse 27-81-1- C,NSW Long. Run 77.551207 joins FORM: WSCAS-03/2012 Page3 of3 1 certify that as a Registered Professional Engineer in the State of North Carolina that I have diligently followed the Division's instructions for classifying waterbodies and that the above classifications are inclusive of the stated project, complete and correct to the best of my knowledge and belief. x, + EIVI� ®F F®1bM WSCAS-03/2012 "xx FORM: WSCAS-03/2012 Page 3 of 3 Kinston Public Services -All Utilities Linds):*City ofKinston Kinston Public Services KinstonlLencir County Address L I Q i pe F ffi OV ya ko Ilk- t.tppam L L o 5 V 75, + 3 3"i • 9/21 /2017 I•.- yw ( 9/21 /2017 Water Resources w Environmental Quality RSD July 26, 2017 ROY COOPER Governor MICHAEL S. REGAN Secretary S. JAY ZIMMERMAN Director City of Kinston DWR ii17-0520 V2 Attn: Mr. Tony Sear, City Manager LENOIR County 207 East King Street Kinston, NC 28501 Subject: On -Site Determination for Applicability to Neuse River Riparian Buffer Rules (15A NCAC 02B .0233) Subject Property/ Project Name: Briery Run Phase IV Sewer Rehab and Project Access Address/Location: South of Intersection of Academy Heights Rd and Airport Rd and extending east to just north of intersection of Briery Run Rd and Wallace Family Rd in Kinston Stream(s) Evaluated: Briery Run and Uts to Briery Run Determination Date: 07/11/17 Staff: Anthony Scarbraugh/Chris Pullinger Determination Type: Buffer: Stream: Z Neuse (15A NCAC 02B.0233) ❑ Intermittent/Perennial Determination ❑ Tar -Pamlico (15A NCAC 02B.0259) Soil ❑ Catawba (15A NCAC 02B .0243) ❑ Jordan (15A NCAC 02B .0267) (governmental Subject and/or interjurisdictional projects) ❑ Randleman (15A NCAC 02B.0250) Survey ❑ Goose Creek (15A NCAC 02B.0605-.0608) 17-0520 V2 A Stream E/I/P* Not Subject Start@ Stop@ Soil USGS Subject - Survey Topo 17-0520 V2 A P X Flag: 17-0520 V2 Flag: 17-0520 X X A Begin V2 A End 17-0520 V2 B P X Flag: 17-0520 V2 Flag: 17-0520 X X - E B Begin V2 B End 17-0520 V2 F I X Flag: 17-0520 V2 Flag: 17-0520 X F Begin V2 F End y7 --'0520V2 G NSP X NSP NSP X 17-0520 V2 H NSP X NSP NSP X *E/1/P/NSP =Ephemeral/Intermittent/Perennial/No Stream Present The Division of Water Resources has determined that the streams listed above and included on the attached map have been located on the most recent published NRCS Soil Survey of LENOIR County, North Carolina and/or the most recent copy of the USGS Topographic map at a 1:24,000 scale and evaluated for applicability to the NEUSE River Riparian Buffer Rule. Each stream that is checked "Not Subject" has been determined to not be at least intermittent or not present on the property. Streams that are checked <� Nothing Compares =._.. State ofNorfh Carolina � Environmental Quality I Water Resources -Water Quality Regional 0lerafions Section-Washingron Regional Office 943 Washington Square Mall, Washington, North Carolina 27889 252-946-6481 CITY OF KINSTON LENOIR County 07/11/2017 Page 2 of 2 "Subject" have been located on the property and possess characteristics that qualify them to be at least intermittent streams. There maybe other streams or features located on the property that do not appear on the maps referenced above but may be considered jurisdictional according to the US Army Corps of Engineers and subject to the Clean Water Act. This on-site determination shall expire five (5) years from the date of this letter. Landowners or affected parties that dispute a determination made by the DWR may request a determination by the Director. An appeal request must be made within sixty (60) calendar days of date of this letter to the Director in writing. If sending via US Postal5ervice: c/o Karen Higgins DWR-401 & Buffer Permitting Unit 1617 Mail Service Center Raleigh, NC 2 7699-1 61 7 If sending via delivery service (UPS, FedEx, etc.): c% Karen Higgins DWR-401 & Buffer Permitting Unit 512 N. Salisbury Street Raleigh, NC27604 This determination is final and binding as detailed above, unless an appeal is requested within sixty (60) days. This determination only addresses the applicability to the buffer rules and does not approve any activity within the buffers. The project may require a Section 404/401 Permit for the proposed activity. Any inquiries regarding applicability to the Clean Water Act should be directed to the US Army Corps of Engineers Washington Regulatory Field Office at (910)-251-4629. If you have questions regarding this determination, please feel free to contact Anthony Scarbraugh at (252)948-3924. Sincerely, UCA Robert Tankard, Assistant Regional Supervisor Water Quality Regional Operations Section Division of Water Resources, NCDEQ cc: Gary Beecher, USACE Washington Regulatory Office (via email) Samir Dumpor, DEMLR WaRO (via email) WaRO DWR File Copy LASERFICHE '1. a v C 1 1 f d f'*� PI ��tf '1 I 1 ff4 1 B 11 1 F '� e let v 1 f d' L�J, °�.��� . - oF�� � l I,�- r� Y ���. . °� l � , I � reef �. [�Qazolhw� Management Commfss Dl�lieion Of Neter Rte. �. . U? � Bullar 4` dais % •7Oli Reviewed by °�` 1� i .,,I � � '� I L. ,r � r � 1 � �I 4.r� L.f L'= 0 � — .. r � •N— ,� II _ i S .. -wv- ry j!e/ ;J t 1.. �Y � .�!1'} 7�r�1-�;S Z C%��r ��,,;�j S ����et��� � V I __ 9 Lf rf �' � az F`r. A k. V y3:. rf� '� _ E S ����et��� � V I __ 9 Lf rf �' � az F`r. A k. V y3:. rf� � 1 m �., J I.� I — � � kY J t t1 � '� -: :i - i � ti .1 � � i ///ff! 1 � - rab f ` PJB -. � �. ..eta k -- ��/� I nI: .. `' _ � l � i+ p�gs�ay�a+�Y; � ;; rJa � - f KL Y<, i � 1V3A V14 �' f i Ya �,-. J&+ !._ h_ Ka �� - - \ \_ � __ —�." _—�. ty ni) — �`` _ _. ..� _.���� �.F ��•�✓r �'� ' � 1 �\�� � � / / J Ise k� �- .'Wa .rut v.a�� 7 !f ,J�;h �� I.I; �� �� �� ��. �= -- J/ ���� N� hr J/ //�/J �" �, Kr ,�..�- �1 ha l�-�� V n 1.� ,.. C� Fr La /// Ka% Wr s �' � J(P. � • 'Y � �' �ecr 161 C 1 e On July 11, 2017, Gary Beecher, from the US Army Corps of Engineers, did a preliminary delineation and evaluation of the site. The evaluation indicated that most of the area in the Sewer line right of way is wetlands. There were areas where the up gradient side of the right of way was not wetlands. It was also noted that the 30 foot wide sewer line right of way had been cleared, and was being maintained because there were only rudimentary wetland plants in the right of way. It was explained that the maintenance was required as part of our Collection System wide permit. There was evidence of ruts where equipment and/or vehicles had been on the right of way. There was also evidence of disturbance because there was soil which was not indigenous to wetlands. This soil is the result of spreading soil from maintenance activities or other activities that required spreading suitable soil for stabilization of the access to the sewer line. Mr. Beecher requested that The City Submit a Nationwide Permit. The Wetlands were investigated by the City of Kinston four different ways. A. The City GIS map has a layer of mapped jurisdictional wetlands. The map is attached with the sewer line on the map, The Project Access Map. The length of sewer line within the wetlands was compiled along with the length of sewer lines not in wetlands. A spread sheet was developed from these measurements, and the spread sheet determined the area of access which was within the wetlands and the area of the access which was not within the wetlands. See map of Access Area and the Spreadsheet Measurements taken from GIS Wetlands Map. According measurements taken from the wetlands map, the sewer line right of way which is within jurisdictional wetlands is 3.16 acres of 10.78 acres or 29.3% of the right of way is in jurisdictional wetlands. B. The City also has a GIS Soils Map with the sewer line on the soils map. A review of the soils information indicates Bibb series and Norfolk series (specifically Norfolk 6 — 10 percent slopes). By definition a hydric soil which is used to delineate wetlands is: "A hydric soil is a soil that formed under conditions of saturation, flooding or ponding long enough during the growing season to develop anaerobic conditions in the upper part' (59 Federal Register 35680, 7/13/94), The Bibb series are Hydric Soils located in Floodplains, typically flat poorly drained, and often flooded. Bibb series support a wetland habitat for both plants and animals. Bibb series soils are definitely a wetland soil. Norfolk series (6 to 10 percent slopes) are not Hydric Soils. Norfolk soils are sloped well drained soils which are not subject to flooding. Norfolk soils do not support wetland plant and animal life. See the Soils Maps of the project area, and the soils information attached. Measurements were made to determine lengths of the sewer line which were in Norfolk Soils and the length of the sewer line which were in Bibb soils. The measurements were compiled into a spreadsheet, (Access Areas (Measurements taken from GIS Soils Map)), which is attached. According measurements taken from the soils map, the sewer line right of way which is in wetland soils is 7.48 acres of 10.78 acres or 69.3% of the right of way is in wetland soils. C. The City has also has a GIS Topographic Map with the sewer line located on it. This Map was used to determine if the sewer line were in a sloped area or a flat area. Although not a true indicator of the presence of a wetland, topography does indicate areas which are sloped, which are generally not associated with wetlands and areas which are flat, which can be generally associated with wetlands. The topographic Map with the sewer line on it is attached. Measurements were made to determine lengths of the sewer line which were in sloped topography, and the lengths of the sewer line which were in flat topography. The measurements were compiled into a spreadsheet, (Access Areas (Measurements taken from GIS Topographic Map)), which is also attached. According measurements taken from the topographic map, the sewer line right of way which is in a flat wetland area is 8.25 acres of 10.78 acres or 76.5% of the right of way is in a flat wetland area. D. From the field Investigation it was noted that the 30 foot right of way had been cleared and was being maintained in accordance with the state regulations and as part of the City's Collection System Permit for sewer outfall lines. The right of way was observed in some places to be cut into the slope of the adjacent hill. When the Sewer line was constructed in the mid 1970's, the soils which were taken from the trench and not put back into the trench were usually spread along the right of way or adjacent area, There was extra soil either because the soil was unsuitable for bedding of a sewer line, or because of the volume of soil which was displaced by the 30" Diameter pipe. In some areas of the cleared right of way there is evidence of plants emerging and presence of animals typical of the soils in a wetland habitat. Adjacent to the cleared right of way there is evidence of all types of trees which inhabit wetlands. See pictures showing Black Gum, Sycamore, Bald Cypress. In addition to many areas of wet hydric soils, there were also areas with localized and wide spread 2 flooding both on the right of way, and adjacent to the right of way. Based upon the field observations, The quantity of Wetlands is closest to the soils map determination. In some cases the disturbance of the right of way has mixed wetland soil and the non -wetland soil to make determination and delineation difficult. For the purpose of this project the entire project access will be treated with the care which would be afforded to all wetlands. In order to support the construction equipment, construction mats will be used. 1. The Plans are prepared from a recent survey, and was correlated with As -Built Plans from 1973. The Plans are for reference purposes only since no digging, filling or construction is proposed. The rehabilitation of this sewer line installed in 1973 will be a "no dig" rehabilitation, and there will be no grading. The existing contours and elevations will be unchanged. Construction Mats will preserve the existing vegetation. If vegetation is damaged, Sections 02850, III, G, 1, 2, and 3, of the Specifications address all of these issues. 2. The As -built drawings from 1973 do not indicate any anti -seep collars, and none are planned to be added to the existing sewer line. 3. The roadway access will be temporary, and all Construction Mats will be removed after construction is complete for each section, Construction Matting will not lay on plant life for weeks thus killing vegetation. See Section 02850, III, E of the Specifications. 4. Since the plans do not propose any changes to topography or drainage characteristics, Overland Flow and the Hydrology of the Wetlands will remain unchanged. 3 ®isturbed Wetlands, Cleared Right of Way Right of wa�� cleared int® tiae s9©goy ���a� �U°�nr�rn Qravc�fi���7s •`�'J# M w � AWL L ` f R- 44 4 f .CV 46 f;� a s :y� y T ML -- "'� rte, z r _ �/q � ate•¢ L..�- �.-u�. ,���� �' - _ i IN Wetland Indication Typical Cypress Flute�7 iir�r�l� Wetland Indication Typical Cypress Knee Paim W4� :. y � ll -77 j NY A IN - \r•`o - - IN IL -IN y .. - ;. c= _ AI IN IN IN - 71 R ty - "`-c ss"` —�c�It / `. I It It 9 a A SIIt IT It IImIII NL _x.. ACCESS AREAS ,d.WS Wetlands Map) ACCESS EASEMENT WETLAND REGULAR WETLAND REGULAR ACRES ACRES ACRES ACRES 0.03 0.01 0.08 0.02 0.05 0.00 0.15 0.00 0.04 0.03 0.12 0.08 0.00 0.01 0.00 0.04 0.07 0.00 0.21 0.01 0.00 0.05 0.00 0.15 0.00 0.03 0.00 0.10 0.00 0.02 0.00 0.05 0.00 0.05 0.00 0.15 0.00 0.09 0.00 0.14 0.00 0.15 :VO.05 0.00 0.20 0.00 0.35 0.00 0.10 . 0.00 0.16 0.00 0.05 0.00 0.15 0.00 0.07 0.00 0.21 0.00 0.06 0.00 0.17 0.00 0.08 0.00 0.23 0.00 0.06 0.00 0.17 0.00 0.08 0.00 0.23 > 0.00 0.04 0.00 0.11 0.00 0.04 0.00 0.11 3 0.00 0.04 0.00 0.12 0.00 0.07 0.00 0.20 0.00 0.05 0.00 0.16 0.00 0.10 0.00 0.30 0.00 0.09 0.00 0.27 0.00 0.06 0.00 0.18 3 0.00 0.10 0.00 0.29 3 0.00 0.05 0.00 0.14 0.00 0.06 0.00 0.18 0.00 0.08 0.00 0.24 3 0.00 0.02 0.00 0.05 3 0.00 0.05 0.00 0.14 3 0.08 0.10 0.23 0.30 0.06 0.05 0.18 0.14 5 0.02 0.13 0.07 0.40 D 0.19 0.00 0.57 0.00 p 0.13 0.00 0.40 0.00 D 0.09 0.00 0.27 0.00 p 0.10 0.00 0.30 0.00 7 0.04 0.16 0.11 0.49 2 0.00 0.12 0.00 0.35 D 0.00 0.10 0.00 0.31 g 0.05 0.04 0.16 0.12 0 0.10 0.02 0.30 0.07 3 1.05 2.54 3.16 7.62 PERCENT WETLANDS PERCENT REGULAR 10 START MANHOLE 84J END MANHOI 84H 84H 84G 84G 84Q 84Q 84F 84F 84E 84E 84C 84C 84D 84D 84B 846 84A 84A 85A 85A 85B 85B 86A 86A 866 86B 86C 86C 86D 86D 86M 86M 86E 86E 86F 86F 86G 86G 86H 86H 861 861 86J 861 86K 86K 86L 86L 87G 87G 87F 87F 87E 87E 87D 87D 87C 87A 179E 179( 179E 179E 179F 179( 1791 1801 E87B B 1801 D 1801 1801 E 1811 D 1811 E 181F 182, A 1828 182 TO1 SoilsMeasurements taken from GIS P.... 11 ACCESS AREAS (Measurements taken from CIS `►opographic Map) 12 IF • I Ibb •.o IF I It I r. IF F IF Ilke �` • • , Ln i, lt_ 180D (ft, 181D 180C' '{ 1806 f 181E 1820 %18�2A IF ILI F, "N' iwlabfif� • lel •�, .. PC LL 84J 84Q 84E - OFF _ - S l 179Frr y i ' 7 NNI • PROJECT � 71 IZ 1NI Legend lands IFIN r Deepwater sfs� stuarine and Marine Welland Freshwater Emergent Weiland I Freshwater Pond LakeiEdIFNI Other IF tos N NI7 iverine Pump Station`¢ 14 IFNSewer Line Ou. Kinston City Limits Sewer Manhole W , - E A "I lop Weiland Acmss WIN-, jAmess .• ' 75 0 FIN .. ','C.. �..,_U& Mb str%°« t,,. wlTrF•LT(`yjl].9 _ yaeialt :. \ 1. .Q .. ,. r�. .�h'. _. Jw. �_ i - Ra -- — iY GoA Re Re on Ly Go GOA ..__- T - GOA \ P�H� ' _. - 0F'aJYYH 1 - GoP _ °Hq Na Ra Pe o l Me — j GA BRIERY RUN PHASE IV Nh t : �� � � ��_ GOA SEWER REHABILITATION Cv P iNo P °me t SOILS MAP M e.Ra RID N, �- 91 Nb /\ 2 7" \ s� � � v j� 4 GOP A°H LY Nb —Ly _ 4 ) � \ - L GO _-- GOA as lmet / A _ i w I REPL A y Ly _ o — Nb GOA i , ex0ro AGA°E. 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Q Y O m d K F ffia" 33 3 �9 "e zQ � €mfg - � zi a Ewoomo a' � p Y 0 x z z o x .� 0$9 E E ry m 0 c O LL xuo o� U U N V (U IU Q Y O m d K F 3 "e e - � a a' � p Y 0 x z z o x .� E E ry m 0 c O LL o� U U N V (U IU Ilo S®H�� II��°®��n��tn®ffi 4°m®rrrm ](.arm®urs (C®nnffi4g�®nIl� I[�c��®rrCr an Bibb Soils (BB) bo craven (Cr) co (Goldsboro (GoA) de Leon (L®) ee Lynchburg (Ly) ff, Norfolk (Na, NbE Nc) go Rains (Ra) h> Wagram (W) ne W®®dnng>t®n (Wn) § �( A . � m mAm aaa - qma\ amw�m, =ea. . M m LENOIR COUNTY, NORTH CAROLINA - SHEET NUMBER 11 ` `SOOOF Lv° l�'- F IJr loins sheet 11 �� \yCo IPiO Ra 11 - .`.A6 L J t 2/ LY Ra I- ( ) Go - - Ga N Nb__ Na iI N=iJ ° - ' C' 1 �' _ NafV\ `l I r Ly I f` �'-Go ti N l f Co `l`�(� t.�!\� N - I`.b LY - Nb �� �J Pz i�..Nb I'�- I - tLY Nb o�fVb E Go G -�� L_ `� 1`la=F\�- �R 1\ . Go Nb NNN - Y . //- _ C -If Re \SLY UID • C- •F;a Ga G LY I -. \ Ly-) _ \ - / .�, f� Nb Go. 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Z Pa - - l l� - `\� ��'- `/ BB-\\ .WcJ/ `, Nb IZ Na.Nb�d _ _l /Wd -EL_ _ - Z _F/ :.Ly W 'Ka IN .� LY �� j�...-Ka - _ \,�+J - .1/ B It`Go � J�/� \� F Nc Ke o JI W sl \ Cr -66 Nb - yf \. N. ._ _ Nb j 7l— /. ✓ Jo Nc '-.��•- \_._- NIC r (Fi `�` _1 —. - ._f - •�.i ,we Na Nc: Nb 4�� Nb 1Jti N`t • Nb Kb fJb Jo IIINlaWd ' Na \ IF. fVb _ vicNa - - Na Nb - Na Ny .OJ Wtl _l. ft y Na LY W� Lie '�"--�/ '/' � \. ) Ke To Go v N LY - G £ Nh Nb �P Nb Ca �/1 ✓ / �� Kb Jo @/'�.f FJ=' ,I Ra • Co L' Q� Kb J f 1 Jo Pr /�a If 'Go \ BB /s Ke I<e L 1 u ugh P -A0 La ill� //� U LY //Pe _ _Co\Co CI 5EP0o- _ LY - fl Nc JO Ka / Jo : ` id P.a '% Na - N\ Na iii/ r Ke �.� I/J• Lv B V Nc Jo c, -In I Win C �!A/ F L-.�-J Ke (,d" I _ _ N b Go Re \ _ ,lGo.- Nb ! eof'hb ,`— `/ 55 \ 'N Ra ( Na •.\ Nb /^ - v\ Nc \ 1 / 1 Ka J. Ka O Pr \ ;` lam_ ! \ Jo LuLu J6Lie \N- NO . Ja / Nb j/ \. LY d��y/---F Nb� `Go ., Cv //Nc Ke Pr /Nei �I'lBE I(b Jo. La /// `Ij 1 Go 1 0\7 81 - \•.69 /N' _ ��p��p LY Nay''' 66'i .1 Nb /%I<a Kb Ke BB I v�_II IVc —Nc ,,J/�V I L'�V -..'Na /""� �' Jo\y Jo 1 Ka ..—_Wn_ pa �� l lNc Na (cut eat).. \. Y / Jo- !lf / -.-- P E.t_ / -. / Nz Nb_ l \�'� BB / Wd N ` f / Ke - (Joins sheet 16) 245000 FEET LENOLR COUNTY, NORTH CAROLINA t' mapping units in that series. Thus, to get full in - nation about any one mapping' unit, it is necessary and to read both the description of the mapping the description of the soil series to which it belongs. An important part of the description of each soil series is the soiPprbfile, that is, the sequence of layers from the surface downward to rock or other under- lying material. Each series contains two descriptions of this profile. The first is brief and in terms familiar toAhe layman. The second is much more detailed and is for those who need to make thorough and precise studies of soils. The profile described in the soil' series is representative for mapping units in that series. If a given mapping unit has a profile in some ways differ- ent from the one described in the series, these differ- ences are stated in the description of the mapping unit, or they are apparent in the name of the mapping .unit. The description of each mapping unit contains suggestions on how the soil can be managed. Color terms are for moist soils unless otherwise stated. Following the name of each mapping unit is a sym- bol in parentheses. This symbol identifies the mapping unit on the detailed soil map. Listed at the end of each description of a mapping unit are the capability unit and woodland suitability group in which the map- ping unit has been placed. The page for the description of each mapping unit can be learned by referring to the "Guide to Mapping Units" at the back of this survey. The acreage and proportionate extent of each map- ping unit are shown in table 1. Many of the terms used in describing soils can be found in the Glossary, and more detailed information about the terminology and methods of soil mapping can be obtained from the Soil Survey Manual (6)? Names in this soil survey do not fully agree with soil maps in.Duplin County. Differences are the result of better knowledge of soils, modifications in series concepts, and the extent of soils within the survey. The Bibb series consists of nearly level, poorly drained soils on flood plains. These soils formed in recent alluvium. In a representative profile the surface layer is dark - gray sandy loam about 12 inches thick. The underlying I extends to a depth of 70 inches., It is mottled, 'Italic numbers in parentheses refer to li terature cited, p. 64. Ta BLE 1. -Approximate acreage and proportionate extent.of the soils Soil Acres Percent =i ecce --ecce-- 8,189 3.2 soils, frequently flooded ecce --ecce-- ------ 3,327 1.3 ' ----------- --------' i,. lton sand, 0 to 6 percent slopes -------------------------ecce-'- 6,910 2.7 --- ----- 1.0 Ghewaela loam, frequently flooded ___ __________ 2,559 Coxville loam --- -- ecce ----------'-----ecce--- - 2,047 Craven fine sandy loam, 1 to 4 percent slopes --------------------------------`--_____________ 511 0.2 Craven.$ne sandy Ioam, 4 to 8 percent slopes --------------------------------- - 5.3 Goldsboro .loamy sand, 0 to Z percent slopes ---------------------------------------- -___ecce- 13,564 _ -- 2,303 0.9 Johns s sandy loam --------- -- - - - - ecceecce----ecce-- -- ecce--- 6,664 2,6 Johns sandy loam ___________________________________________________________ -----ecce-- --- 7,934 361 Johnston soils 4,862 .9 Kalmia Ioamy sand, 0 to 2 percent slopes ______________ 3,327 1.3 $almia Ioamy sand, 2 to �6 percent slopes ---------------ecce-- 5 680' 2.2 Kenansville loamy sand, 0 to 6 percent slopes ----- -------- _____ 4,094 1.6 Kinston loam, frequently flooded 7,678 3.0 Lakeland sand, 0 to 6 percent slopes --------------------------------------------------------- Leaf loam '- -- ----ecce--=-------- 3,327 1.3 1;279 Lenoir loam ---------- -- .4,094. 1.6 ------------------------------- --- Leon sand-----------ecce----ecce---ecce----ecce-- ecce 5,586 '2.3 Lumbee sandy loam ____ '------------------------------ Lynchburg sandy loam ecce- __ ---- -- ecce-- 12,254 4.8 767 D.3 Meggett fine sandy loam Murville fine sand ------- � 2,303 0• eccecentslopes --ecce-------ecce-----ecce-- --ecce---ecceecce-- 17,659. 6.9 Norfolk loamy sand, 0 to 2 percent slopes----------------- -------ecce---ecce-- ---'-ecce-- . - ecce 18,141 Norfolk loamy sand, 2 to 6 percent slopes -----------------------------------------ecce-- 3,583 1.4 Norfolk loamy sand, 6 to 10 percent slopes ----------------------------------- - ' '--' Pactohis loamy sand .----- ------------'-------ecce-------ecce---ecce---ecce-- __ 4,360 1.7 4,862 •9 Pamlico muck---------------------------------------.--------ecce-------------ecce--ecce-- 5,118 2.0. Pantego loam _ Poealla loamy sand, 0 to 6 percent slopes----------------------------------ecce-------'ecce 28,685 11.2 . _______ 2,815' 1.1 Portsmouth loam Rains sandy loam ecce= -ecce-- ecce-------- 18,683 7.3 ---------------------- ---ecce-- 11,OD5 4.3 Starlings •loamy sand ---------------`"-- --------------------------- ' '__--- 9,725 ... 3.8 Torhunta loam --- Umbria Ochraqualfs - -- ecce-- ----------------ecce--ecce-- ecce--ecce------ecce-- 611 0.2 --- - - - 8,189 3.2 Wagram loamy sand, D to 6 percent slopes -------------------------------------------------- Wagram loamy sand, 6'to 10 percent slopes .-_--ecce-- - __ 2,303 0.9 - ----------------------------------- 2,559 1.0 Waeram loamy sand, 10 to 15 percent slopes --------------- ----------- ------------ -- 511 6.2 ' F oam loamy send, Y to 6 perpent Slopes _ ________________ 7 B7g 3.0 .mgton loamy sand _______________________________________________ ------------- m..+moi255,936 100.0 ----------------- ---ecce- SOIL SURVEY dark -gray -and gray sandy loam in the upper part and d grayish -brown loamy sand in the lower part. Bibb soils are low in natural fertility and content of organic matter. Permeability is moderate, and avail- able water capacity is medium. Shrink -swell potential is dow. The seasonal high water table is at the surface. These soils flood frequently for brie£•.periods. Flooding is more frequent in winter and in spring. ATearly all of the.acreage is wooded. A small acreage is cultivated and pastured. Representative profile o£ Bibb sandy loam from an area of Bibb soils, frequently flooded, in a wooded area 4 miles south of Hugo, 0.3 mile north of inter- section of State Roads 1700 and 1731 and 50 feet east of bridge on State Road 1731: Al -0 to 12 inches, dark -gray (10YR 4/1) sandy loam; few, fine, faint, dark reddish -brown stains around.: old roots; moderate, medium, granular -structure; very friable; many large roots; very strongly acid; clear, wavy boundary. Clg--12 to 45 inches, mottled, dark -gray (IGYR 4/1) and gray (10YR 5/1) sandy loam; few thin strata of loam and loamy sand; few, fine, distinct, yellowish - brown and brown mottles; massive; very friable, slightly sticky and slightly plastic; few fine and medium roots; very strongly acid; gradual, wavy boundary. G2g--45 to 70 inches, grayish -brawn (10YR 5/2) loamy sand; massive; very friable; strongly acid. Reaction is very strongly acid or strongly acid unless the soils are limed. The A horizon is dark -gray or dark grayish - brown sandy loam, loam, or loamy sand. The C horizon is dark -gray, gray, grayish -brown, or fight brownish -gray sandy loam or loam. In places this horizon has thin strata of sand and silt loam. The C horizon, below a depth of about 45 inches, is Ioamy sand or sand. Few to common brown mottles are in the upper part of the C horizon. Bibb soils, frequently flooded (BB).—These soils are in narrow drainageways. Slopes are less than 1 per- cent. The surface layer is sandy loam, loam, or loamy sand. In a few of these soils the underlying layer is nonacid, and marl is at depth of 4 to 7 feet. The areas are long and narrow and range from 30 acres to sev- eral hundred acres in size. They are generally larger than those mapped elsewhere in the county, but map- ping has been controlled well enough to make the in- terpretations for the anticipated uses. Included 'with these soils in mapping are several areas of Kinston and Johnston soils. Infiltration is moderate, and runoff is slow. Water is ponded in places. If properly drained, these soils are suited to a few locally grown crops. Surface and subsurface drainage and protection from floods are needed for all Crops. Because. of lack of suitable outlets, construction of drainage systems is difficult in places where marl un- derlies these soils. Water ponding on the surface, mod- al high te• table and crate permeability, a season g water frequent flooding are the main limitations in the use and management of these 'soils. Capability subclass Vw, frequently flooded; woodland suitability 2w9. Blanton sand, 0 to• 6 percent slopes soil is on broad, smooth and slightly rounded divides. The areas range from about 5 to 50 acres in size and are about as broad as they are long. Included witb this soil in mapping are -small areas Of Wagram, Lakeland; and Pocalla soils. In places Ion narrow areas of Leon soils are included at the foot of slopes. Infiltration is rapid, and runoff is slow., Blanton Seraaa;3 The Blanton series consists of nearly level to gently sloping, well -drained soils on uplands: . In a representative profile the surface layer is lig brownish -gray sand about 3 -inches thick. The subst face layer. is very pale brown sand about 52 inch thick. The subsoil is 43 inches thick. The upper part brownish -yellow sandy loam. The middle part yellowish -brown sandy clay loam -that is mottled wi brown and gray.- The lower part .is light yellowis brown sandy clay loam that is mottled with brown ai gray. Below this layer; to a depth of 120 inehes, is pal brown loamy sand that is mottled with brown ai gray.. Blanton soils are very low in natural fertility ar content of organic matter. Permeability is moderat and.available water capacity is very low.. Shrink-swe potential is low. The seasonal high water table remain below a depth of about 5 feet. Most of the acreage is wooded. The rest is cultivate or used for nonfarm purposes. Representative profile of Blanton sand, 0 to 6 perces SI in a wooded area 1 mile southwest of LaGrange 0.2 mile south of intersection of U.S. Highway 70 am State Road 1323, and 50 feet east of State Road 1323 Al -6 to 3 inches, light brownish -gray (10YR 6/2) sand very weak, medium, granular structure; very fri able; common roots; very strongly acid; gradual wavy boundary. A2-3 to 55 inches, very pale brown (10YR 7/4) sand single grained; loose; few lenses of light -gray sant in the lower part; very strongly acid; gradual wavy boundary. B1-55 to 63 inches, brownish -yellow (10YR 6/8) sand3 loam, weak, fine, subangular blocky structure; very friabie; very strongly acid; gradual, wavy. bound. ary. B2t-63 to 80 inches, yellowish -brown (10YR 5/8) sandy clay loam• common, medium, distinct, strong -brown (7.5 -YR 518) mottles and few, medium, distinct; gray (SOYR 6/1) mottles; weak, fine, subangular blocky structure; friable, slightly sticky and slight- ly plastic; thin, discontinuous clay films. on faces of peds; very strongly acid; gradual, wavy bound- ary. B3-80 to 98 inches, light yellowish -brown (10YR 6/4) sandy clay loam; few, medium, distinct, strong - brown (7.5YR 5/8) and gray (10YR 5/1) mottles; weak, fine, subangular blocky structure; friable, slightly sticky and slightly plastic; very strongly acid; gradual, wavy boundary. C-98 to 120 inches, pale -brown (JO'YR 6/3) loamy sand, few, medium, distinct, strong -brown (7.5YR 516) and gray (16YR 611) mottles; massive; very, fri- able; few pebbles; strongly acid. The solum is more than 60 inches thick. Reaction is very strongly acid or strongly acid unless .the soils.are limed. The Ap and Al horizons are grayish brown, light brownish gray, or light gray. The A2 hori,00s.very pale brown or P brown. The B horizon is light yellowish -brown, brown- ish -yellow, yellowish -brown, or strong -brown sandy clay loam or sandy loam that is mottled with brown, gray, and red. The C horizon is loamy sand, sandy loam, or sandy clay loam, SOIL SURV>;Y erately slow, and available water capacity is medium to high. Shrink -swell potential is moderate. The sea- sonal high water table is at the surface. Most of the acreage is wooded. The rest is cultivated and pastured. Representative profile of Coxville loam, 2 miles southeast of LaGrange,' in a cultivated field, 0.4. mile east of intersection of U.S. Highway 70 and State Road 1327, 0.3 mile southeast of State Road 1327, and 20 -feet southwest of farm road: �` Ap—D to &inches, dark -gray .(lOYR 4/1) loam; weak, medium, granular strueture;�friahle; common me- ilium roots; medium acid; abrupt, smooth boundary. Blg—S to 12 inches, light brownish -gray' (IOYR 6/2) loam; £ew, medium, distinct, light yellowish -brown (10YR 6/4) mottles; weak, fine, subangular bloclry strne- ture• friable; few fine roots; fevtores filled with dark -gray loam; very strongly acid; clear, wavy boundary � 10YR 6 1 ela loam; com- B21tg-12 to 29 inches, gray ( /) y man, medium, distinct, brownish -yellow (lOYR 6/0) mottles; weak, fine, angular blocky structure; firm, sticky and plastic; £ew fine roots; thin, discontin- uous clay films on faces of peds and on pore walls; very strongly acid; gradual, wavy boundary. B22tg-27 to 40 inches, gray (lOYIt 6/1) clay loam; com- mon, coarse, distinct, brownish -yellow (10YR 6/0) mottles and few, fine, prominent, red mottles; weak, fine, angular blocky structure; firm, sticky and plastic; thin, discontinuous clay films on faces of peds and on pore walls; very strongly acid; gradual boundary. Bag --46 to 62 inches, gray. (lOYR �6/1)'clay loam;�com- mon, inedium, distinct, brownish -yellow (IOYR 6/0) mottles and few, medium, prominent, red (2.5YR 4/3) mottles; weak, fine, angular blocky structure; firm, sticky and plastic; thin clay films on pore walls; very strongly acid• gradual, wavy boundary. Cg -62 to 75 inches, light -gray (10YR 7/1) sandy clay loam �: that has lenses o£ sandy loam; common, medium, iaint,_�pale-brown {lOYR 6/3) mottles; massive; friable, slightly sticky and slightly plastic; very strongly acid. The solum is 60 inches to -more than SD inches thick. Re- action is very strongly acid or strongly acid unless the soils are limed. The A horizon is gray, dark gray, or very dark gray. The very dark gray part of the A horizon, if present, ' is less than 8 inches thick. The B horizon is light brownish - gray or gray loam, clay loam, or sandy clay that is mottled with yellow, red, and brown. The C horizon is sandy clay, sandy clay loam, or sandy loam. �®gellle Hoasun (Co). This soil is on broad, smooth flats on stream terraces and in shallow depressions on upland intersiream areas. Slopes are less than 2 per- cent. The areas are'generally small and narrow. Included with this soil in mapping are small areas of soils that have a surface layer of sandy loam. Also included are a few areas of Rains, Lumbee, and Leaf SO11S. Infiltration is slow, and runoff is slow. Water ponds in some places. This soil is diifieult to keep in good filth and can be worked within only a narrow range of moisture content. This soil, if drained, is well suited to a few locally grown crops, mainly corn and soybeans. Surface and subsurface drainage is needed forwatertponding on the Moderately slow permeability, surface, and a seasonal high water table are the main limitations in the use and management of this soil., "apability unit IIIw-2, drained; capability subclass TVw, undrained; woodland suitability group 2w9. The Craven series consists of nearly level.to sloping, moderately well drained soils on uplands and stream terraces. In. a representative profile the surface layer is grayish -brown fine sandy loam about 8. inches thick. The subsurface layer is pale=brown fine sandy loam about 2 inches thick. The subsoil is 42 taches thick. The upper part 'is light yellowish -brown loam, the middle -part is yellowish -brown and light yelloy✓ish- brown clay that is mottled with brown and gray, and the lower part is gray clay loam that is mottled with brown and red. Below the subsoil, to a depth of about 80 inches, is gray sandy clay loam that is mottled with yellow and brown. Craven soils are medium in natural fertility and low in content of organic matter. Permeability is slow, and available water capa'eity is medium. 'Shrink -swell po- tential is moderate. The seasonal high water table remains at a depth of about 30 inches.. About one-half of the acreage is wooded. Most of the rest is cultivated, but a small part of it is pastured. Representative profile of Craven fine sandy loam, 1 to 4 percent slopes, 9 miles northeast of Sinston, 200 feet east of intersection of State Roads 1804 and 1803 and 25 feet north of State Road 1803 e Ap-0 to 8 inches, grayish -brown (10YR 5/2) fine sandy loam; weak, medium, granular structure; very frr able; many fine roots; medium aeid;'abrupt, smooth bonndaiy. A2-3 to 10 inches, pale -brown (lOYR 6/3) fine sandy loam; weak, medium, granular structure• very fin- able; many fine roots; strongly acid; clear, wavy boundary. B1-10 to 13 inches, light yellowish -brown (lOYR 6/4) loam; weak, fine, subangular blocky structure; fri- able; common fine roots; very strongly acid; clear, wavy boundary. B21t-13 to 23 inches, yellowish -brown (IOYR 6/8) clay few, medium, faint, strongbrown (7.5YR 5/3) mottles• moderate, fine, angular bIoaky structure; very firm, sticky and very plastic• thin clay films on £aces of peds; very strongly acid; gradual, wavy boundary. B22t-23 to 37 inches, light yeIIawish-brown (IOYR 6/4) clay; common, medium, distinct, gray (lOYR 6/1) and strong -brown (7.5YR�5/3) mottles• moderate; fine, angular blocky structure; very firm, sticky , ' and very plastic; thin clay films on £aces' of peds and in pores; very strongly acid; gradual, wavy boundary. Bag --37 to 52 inches, gray (YOYR 6/1) clay loam; common, medium, distinct, yellowish -brawn (1DYR 5/8) mot- tles and few, medium, prominent, red (2.5YR 4/S) mottles; weak, fine, angular 'blocky structure; very firm, sticky and plastic; few fine flakes of mica; thin clay films ir} pores; very strongly acid; grad- ual, wavy �bonndary. Cg -52 to 80 inches, gray (10YR 6/1) sandy clay loam that has lenses o£ sandy loam and sandy clay• common, coarse, distinct, brownish -yellow (10Y.It 6/3) mottles and few, medium, distinct, strong - brown (7.5YR 5/3) mottles; massive; friable, sticky ' and plastic; few fine flakes of mica and soft min- ' eral grains; very strongly acid The solum is 40 to OD inches thick. Reaction is very strongly acid or strongly acid unless the soils are Limed. The Ap and Al horizon is grayish brown or dark gray. The B horizon is yellowish brown or light .yellowish brown and is mottled 'with gray and brown m the upper part. It is gray and mottled with few to common mottle$ of brown, LENOIR COUNTY, NORTH CAROLINA 9 gray, and red in the lower part. The gray mottles are be- tential is low. The seasonal high water table is at a tween 18 and so inches below the surface. The C horizon depth of about 30 inches. is commonly sandy clay loam or sandy clay. Most of the acreage is cultivated. The rest is pas - Craven fine sandy loam, 1 to 4 percent slopes (Cr).—' tured or wooded or is used for nonfarm purposes. This soil is on gently sloping sides of divides. The areasRepresentative profile of Goldsboro loamy sand, 0 in 5 to 30 acres in si are size. This soisouth of Hugo *in a cultis-s l has he profile range shaped and sc ibed s Tepre enta- vated field,r0 7 m le east of into se t on of State Roads five for the series: 1726 and 1727 and 50 feet north of State Road 1727: Included with this soil in mapping are a few areas Ap-0 to 8 inches, grayish -brown (10YR 5/2) loamy sand; of eroded soil and some areas of soil where the slope weak, medium, granular structure; very friable; is less than 1 percent. Also included are small areas of few roots; strongly acid; abrupt, smooth boundary. Lenoir, Goldsboro, and Johns soils and a few short A2-8 to 12 inches, pale -brown (loYR 6/3) loamy sand; weak, medium, granular structure; very friable; narrow strips of Bibb soils. Some delineations have a few roots; few pores filled with grayish -brown few small spots of wet soils in depressions. A wet spot loamy sand from the surface layer; very strongly symbol is used to show these spots. acid; clear, wavy boundary. Infiltration is moderately slow, and runoff is slow B1-12 to 16 inches, light yellowish -brown (10YR 6/4) sandy loam; weak, fine, subangular blocky strue- to medium.tune; friable;" few fine roots; very strongly acid; This soil is well suited to all locally grown crops and clear, wavy boundary: small grain. Practices are needed to control runoff and B21t--16 to 28 inches, yellowish -brown (10YR 5/6) sandy erosion. Water collects in the low Spots in fields for clay loam; weak, fine, subangular blocky structure; brief periods after heavy rainstorms. Drainage is friable, slightly thhin discontinuous 6layand lyfilmsson fay s needed in places where the particular use requires_a of peels; very strongly acid; gradual, wavy bound - well -drained condition. ary. Moderate shrink -swell potential, slow permeability, 'B22t-23 to 45 inches, pale -brown (10YR 6/3) sandy clay and runoff are the main limitations in the use and man- loam; common, medium, distinct gray (10YR 6/1) agement of this soil. Capaliiility unit lIIe-1• woodland and brownish -yellow (10YR 6/8) mottles and few, ' medium, distinct, strong..brown (7.6YR 5/8) mot - suitability group 3w2. ttes; weak, fine, subangular blocky structure; fri- Craven fine sandy loam, 4 to 8 percent slopes (Cv).— able, slightly sticky and slightly plastic; thin, dis- This soil is between the gently sloping areas and flood continuous clay films on faces of Peds; very plains or stream terraces. The areas are narrow and Bsg-45 stod68linches, gray HIYR s/ jus sandy clay loam; l.�^g and range from 5 to 50 acres in size, - common, medium, distinct, brownish -yellow (10YR icluded with this `soil in mapping are a few areas of 6/8) and red (2.5YR 4/8) mottles; weak, fine, sub- sods that have a surface layer of clay , and Also in - angular blocky structure; friable, slightly sticky eluded are small areas of Bibb, Norfolk, and Wagram and slightly plastic; thin, patchy clay films in soils. Infiltration is slow, and runoff is rapid. This soil is suited to all locally grown crops, but the short length and' gradient of the slopes limit the use of -this soil for row crops. Runoff causes a hazard of erosion if this soil is cultivated, and practices are needed to control runoff and erosion. Moderate shrink -swell potential, slow permeability, runoff, and slope are the main l mitations in the use and management of this soil. Capability unit IVe-1; woodland suitability group 3w2. Goldsboro Series The Goldsboro series consists of nearly level, mod- erately well drained soils on uplands. In a representative profile the surface layer is gray- ish -brown loamy sand about 8 inches thick, The subsurface layer is pale -brown loamy: sand about 4 inches thick. The subsoil_ is 56 inches, thick. The upper part. is light yellowish -hr sandy loam, the middle part is yellowish -brown. and pale -brown ,and brown, loam that is mottled with gray, yellow, and the Iower part is gray sandy clay "loam that is mottled with yellow and.red. Below the subsoil, to a depth of 80 inches, is light -gray sandy clay loam that is --�ottled with•red and brown. ldsboro soils are low in natural fertility and con- tenu of organic matter.. Permeability is moderate, and available water capacity is medium, Shrink -swell Po - pores; very strongly acid; gradual, wavy boundary. Cg�68 to 80 inches, light -gray (lOYR 7/1) sandy clay loam that has thin lenses of sandy clay and sandy loam; few fine, prominent, red mottles and common, medium, pale -brown (10YR 6/3) mottles; friable, alightly sticky and slightly plastic; very strongly acid. The solum is 60' to about 85 inches thick. Reaction is very strongly acid or strongly acid unless the soils are limed. The Ap or Al horizon is grayish brown or dark grayish brown. The B horizon is sandy clay foam or sandy loam. The' B1 and B2 horizons are pale brown, light yellowish brown, or yellowish brown and are mottled with gray, yellow, and brown. The C horizon is commonly sandy clay loam or sandy loam. Goldsboro loamy sand, 0 to 2 percent slopes (Go).— This soil is near shallow drainageways on broad, smooth divides. The areas are nearly as broad as they are long and range from 10 to 30 acres in size: -. Included with this soil in mapping are a few areas of soils that have a surface layer of sandy loam and very fine sandy loam and some . that have . a siltier subsoil than this soil. Also included are a few small areas of Norfolk and Lynchburg soils. Infiltration is moderate, and runoff is slow. This soil is well suited to all locally grown, crops and is used mainly for corn, soybeans, tobacco, small grain, P plants, and truck crops. If drained, it is well sfi te4 to tobacco aces where the type f use requires a well. -s, neededainage is drained condition. A seasonal high water table is the main limitation in 10 SOIL SURVEY lt'.sgure 3.—Tobacco growing on Goldsboro loamy sand. the use and management of this soil. Capability unit IIW wcodIand suitability group 2w8. G>rafer ®><n S�x°a�� The Grifton series consists of nearly level, poorly drained soils on uplands and stream terraces. In a representative profile the surface layer is dark - gray sandy loam about 8 inches thick. The subsurface layer is grayish -brown sandy loam about 4 inches thick. The subsoil is 46 inches thick. The upper part is light brownish -gray sandy loam that is mottled with gray. The middle part is gray sandy clay loam or sandy loam that is mottled with yellow and brown. The lower part is gray loamy sand. Below the sub- soil, to a depth of 70 inches, is greenish -gray marl that crushes to sandy Ioam. Grifton soils are low in natural fertility and content of organic matter. Permeability is moderate, and available water capacity is medium. Shrink -swell po- tential is low. The seasonal high water table is within 10 inches of the surface. Most of the acreage is wooded. The rest is cultivated or pastured. Representative profile of Grifton sandy loam in a cultivated field 7 miles southeast of Kinston, one-, ( 'ourth of a mile southeast of intersection of State Roads 1915 and 1903 and south of State Road 1915: Figure 4.-751e laid out Por installation oA Goldsboro loamy sand. Ap-0 to s inches, dark -gray (10YR. 4/Y) sandy loam; weak, medium, granular structure; very friable; common fine roots; strongly acid; abrupt, smooth boundary. A2-8 to 12 inches, grayish -brown (IOYR 5/2) sandy loam; weak, medium, granular structure; very friable; common fine roots; strongly acid; clear, wavy. boundary. BIg--12 to 15 inches, light brownish -gray (IOYR 6/2) sandy loam; common, medium, faint, gray (10YR 6/1) mottles; weak, fine, subangular blocky struc- ture; very friable; common fine roots; strongly acid; gradual, wavy boundary. B2ltg-15 to 32 inches, gray (10YR 6/1) sandy clay loam that has lenses of sandy loam; common, Res, dis- tinct, reddish-yellow mottles; weak, fine, subangular blocky structure; friable, slightly sticky and slightly plastic; common .fine and medium pores; thin, discontinuous clay, films on faces of peds and on pore walls; strongly acid; gradual, wavy boundary, B22tg--32 to 40 inches, gray (10YR 6/1) sandy loam that has lenses of sandy clay loam and loamy sand; _ common, coarse, distinct, yellowish -brown (IOYR , and m sli ghtly plastic; common fine and mediuF pores; neutral; gradual, wavy boundary. B3g�0 to 58 inches, gray (YOYR 6/Y) loamy sand that has thin lenses of sandy clay loam; massive; fri- able; moderately alkaline; gradual, wavy bound- ary. IIGg=58 to 70 inches, greenish -gray (5GY 5/1) marl that crushes to sandy loam that has thin lenses of clay; massive; friable; moderately alkaline. 16 SOIL SURVEY sticky and very plastic; few fine roots; 'thin clay films on faces of peds; very strongly acid; clear, wavy.boundary. B22tg-21 to 48 inches, gray (10YR 6/1) clay; many, me- dium, distinct, brownish -yellow (IOYR 6/8) mottles and common, medium, prominent, red (2.5YR 4/8) mottles; moderate, fine, angular blocky structure; very firm, sticky and";very plastic; thin clay fibres ,on faces of Peds .and in pores; very strongly acid;' Bag -48 to 62 inches, gray (lOYR 6/1) clay; many, medium, ,distinct, brownish -yellow (joYR 616) mottles and .few, medium, prominent, red (2.5YR 4/8) mottles; moderate, tine, angular blocky structure; very firm, sticky and very plastic; thin clay films in pores; very strongly acid; gradual, wavy bound- ary. Cg -62 to 75 inches, gray (10YR 5/1) clay loam that has ,thin lenses of sandy clay loam; few, medium, dis- tinct to prominent, brownish -yellow (10YR 6/6) and strong -brown (7.5YR 5/8) mottles; massive; firm, sticky and very plastic; very strongly acid. The solum is more than 60 inches thick. Reaction is very strongly acid or strongly acid unless the soils are limed. The Al or Ap horizon is dark gray or dark grayish brawn. The B1 horizon is pale brown, light yellowish brown, or brownish yellow and mottled with yellow and gray in the upper part. Below a depth of about 21 inches, it is gray and mottled with yellow, brown, and red. The B horizon is clay • to clay loam. The C horizon is clay loam on sandy clay loam. The A horizon and the Bl horizon, if present, are slightly thicker than -the defined range for the series. The contrast in texture between the surface layer and the subsoil is also greater. Thase differences do not alter the usefulness or be= • havior of the soils. Lenoir lloain (Ln).—This soil is on broad, smooth divides near shallow drainageways. Slopes are 0 to 2 percent. The areas are nearly as broad as they are long and range from 10 to 40 acres in size. Included with this soil in mapping are a few areas of soils that have a surface layer of sandy loam. Also included are small areas of Leaf and Craven soils. Inilitration and runoff are slow. The soil is difficult to keep in good tilth and can be worked only over a narrow range of moisture content. The main tree species is Ioblolly pine. If drained, this soil is suited to a few locally grown crops, mainly coin and soybeans. Surface and subsurface drainage is needed for most crops. Adequate drainage is diffi- cult to obtain because of the slow permeability. Prac- tices to improve the soil structure and tilth are needed to obtain good drainage and aeration. . Slow permeability, moderate shrink -swell potential, water ponding on 'the surface, and a seasonal high crater table are the main limitations in the .use and management of this soil. Capability unit IIIw-4; wood- land suitability group 2w8. The Loon series consists of nearly level, somewhat poorly drained soils on uplands and stream terraces. in a representative profile the surface layer is dark - gray sand about 4 inches thick. The subsurface layer is light -gray sand about 10 inches thick. The subsoil is sand 17 inches. thick. The upper part is black and the lower part is dark brown. The underlying layer, to a depth of about 72 inches, is light brownish -gray loamy I and in the upper part and dark reddish -brown and grayish -brown sand in the lower part. Leon soils are very low in natural :fertility and con- tent of organic matter. Permeability is rapid to mod-. erately rapid, and available water capacity .is 'low. Shrink -swell potential is very low. The seasonal high water table is at a depth of about 1S inches. Most of the acreage is wooded. Representative profile of Leon sand in an idle fieldh5 miles eastbf Pink Hill, 0:6 mile east of the intersection" of State Roads 1105 and 1I1S; and 25 feet south of State Road 1105: Al -0 to 4 inches, dark -gray {lOYR 4/1) sand; single grained; loose; about 2P percent of grains coated with organic matter; also few fine particles of or- ganic matter; common large roots; very strongly acid; clear, wavy boundary. A2-4 to 14 inches, light -gray (I6YR 7/1) sand; single grained; loose; common roots; very strongly acid; abrupt, wavy boundary. B2h-14 to 19 inches, black (5YR 2/1) sand; massive; fri- able; weakly cemented; thin humus coating on grains; very strongly acid; clear, wavy boundary. Bah -19 to 31 inches, dark -brown (7.5YR 3/2) sand; mas- sive; friable; weakly cemented fragments of dark reddish brown; thin humus coatings on grains; very strongly acid; clear, wavy boundary. C1— 31 to 37 inches, light brownish -gray (10YR 6/2) loamy sand,-' single grained; loose; very strongly acid; clear, wavy boundary. C2--37 to 58 inches, dark reddish -brown (5YR 3/2) sand; massive; friable; weakly cemented; thin humus coatings on grains; very strongly acid; clear, wavy boundary. C3-58 to 72 inches, grayish -brown (10YR 5/2) sand; . 'single grained; very friable; very strongly acid. These soils are sand or fine sand to a depth of 72 inches or more: Reaction is very strongly acid or extremely acid unless the soils are limed. The Al horizon is dark gray or very dark gray. The A2 horizon is light gray or white. The Bh horizon is black, dark reddish -brown, or dark -brown sand or loamy sand. The C horizon is loamy sand to sand. L¢on sand (Lo) This soil is on the outer rims of I depressions and on broad, smooth interstream divides. Slopes are 0 to 2 percent. The areas are ir- regularly shaped and range from 5 to 25 acres in size. Included with this soil in mapping are a few areas of 'soils that have a surface layer of fine sand. Also included are. a few small areas of Woodington, Pacto= I is; Murville, and Stallings soils. Infiltration is rapid, and runoff is very slow. This soil is poorly suited to most locally grown CT The main tree species are longleaf pine and turkey oak. Because of the coarse texture and the humus hardpan subsoil within 80 inches of the sur- face, this soil is very poorly suited to cultivation except for specialized craps, such as blueberries. Leaching of plant nutrients, hardpan subsoil, and a seasonal high water tablez are the main limitations in the use and management of this soil'. Capability unit IVw 1; woodland suitability group 4w2. The Lumbee series consists of nearly level, poorly chained soils on stream terraces. In a representative profde the surface layer is dark - gray sandy loam about 7 inches thick. The subsurface layer is light brownish -gray sandy loam about 5 inches thick. The subsoil is 26 inches thick. The upper part is light brownish -gray and gray sandy clay loam that is LENOIR COUNTY, NORTH CAROLINA Atled with brown and yellow, and the lower part is y sandy loam that is mottled with brown. Below the supsoil, to a depth of about 65 inches, is light brownish - gray sand. Lumbee soils are low in natural fertility and content of organic matter. Permeability is moderate, and avail- able water capacity is medium. Shrink -swell potential is water table is at the surface. Most of the w. The acOe age al hwooded. The rests cultivated and pastured. Representative profile of Lumbee sandy loam in a cultivated field 2.5 miles southeast of Jenny Lind, 0.7 mile north of intersection of State Roads 1333 and 1324, and 50 feet west of State Road 1333: Ap-0 to 7 inches, dark -gray (10YR 4/1) sandy loam; weak, medium, granular structure; very friable; common fine roots; medium acid; abrupt, smooth boundary. A2-7 to 12 inches, light brownish -gray (10YR 6/2) sandy loam; weak, medium, granular structure; very fri- able, common fine roots; common pores filled with dark -gray material from layer surface; strongly acid; gradual,, wavy boundary.. Blg-12 to 14 inches, light brownish -gray (10YR 6/2) sandy clay loam; few, medium, faint, light yellowish -brown (10YR 6/4) mottles; Weak,'fine, subangular blocky structure; friable, slightly sticky and slightly plastic; few pores filled with dark -gray surface soil; very strongly acid; gradual, wavy nounaary. B2tg-14 to 34 inches, gray (10YR 6/1) sandy clay loam; few, Sue, distinct, brownish -yellow and stxong- brown mottles; weak, fine, subangular blocky stric- ture; friable, slightly sticky and slightly plastic; diseentinuous clay films on faces of peds; :few fine flakes of mica; very strongly acid; gradual, wavy boundary. B3g--34 to 38 inches, gray (IOYR 611) sandy loam; com- mon, medium, faint, pale -brown (10YR 6/3) met- tles; weak, fine, subangular blocky structure; friable disco tinuoustcllay fily lms ndfaces of peds; fewfine flakes of mica; very strongly acid; gradual; wavy boundary. Cg -38 to 66 inches, light brownish -gray (10YR 6/2) sand le grainedat ; loose; few hin few lenses fine fakesoamy of mica; "trougly acid. The solum, is about 38 inches thick but ranges from 26 to 40 inches. Reaction is very strongly acid or strongly acid unless the soils are limed. The Ap or Al horizon is dark gray or dark grayish brown. The B horizon is gray, light brownish -gray, or light -gray sandy clay loam or sandy loam that is mottled with yellow and brown. The C horizon is sand or loamy sand. 1Lumbee sandy loam (Lu).—This soil is in shallow dramageways separated by low, broad ridges. Slopes are 0 to 1 percent. The areas are long and variable in width and range from about 10 to 100 acres in size. Included with this soil m mapping are a few areas of soils that have a' surface layer of very fine sandy loam and loamy sand. Also included are a few small areas of Coxville, Portsmouth, Woodington, I and Johns soils and areas of soils that have a thicker subsoil. Infiltration is moderate, and runoff is slow. If drained, the soil is suited to a few locally grown creps,'ch%efly corn and soybeans. Surface and sub- s77„4ace drainage is needed before this soil can be vated or pasiured. The sandy substratum is un- sianle in ditchbanks and is a limitation to installation and maintenance of drainage systems. Water ponding on the surface and a seasonal high water table are the main limitations in the use and management. of this soil. Capability unit II1W-8; wood- land suitability group 2w9. ? UZM r i' i ,,,. The Lynchburg series consists of nearly level, some- what poorly drained soils on uplands. In a representative profile the surface layer is dark - gray sandy loam about 8 inches thick. The subsurface layer is light brownish -gray sandy loam about 4 inches thick. The subsoil is 54 inches thick. The upper part is pale -brown sandy clay loam that is mottled with gray and yellow. The lower part is gray sandy clay I that is mottled with yellow -'and red. Lynchburg soils are low in natural fertility and con- tent of organic matter. Permeability is moderate, and available water capacity is medium. Shrink -swell po- tential is low. The seasonal high water table is at 'a depth of about 18 inches. About half the acreage is cultivated or pastured. The rest is wooded. Representative profile of Lynchburg sandy loam in a cultivated field 0.1 mile north of Savannah School, 0.1 mile northwest of intersection of State Roads 1723 and 1727, and 50 feet west of State Road 17M Ap-0 to 8 inches, dark -gray” (10YR 4/1) sandy loam; weak, medium, granular structure; very friable; common fine roots; medium acid; abrupt, - smooth boundary. A2--8 to 12 inches, light brownish -gray (10YR 6/2) sandy loam; weak, medium, granular structure; very fri- able; common 'fine roots, many pores filled with dark-erav material from Ae surface layer; strongly B1-12 to 15 inches," pale -brown (10YR 6/3) sandy clay loam; few, Tine, faini, light brownish -gray mottles; weak, fine, subangular bloehy structure; friable; common fine roots; few pores filled with dark -gray material from the surface layer; very strongly acid; clear, wavy boundary. B21t-15 to 21 inches, pale -brown (10YR 613) sandy clay loam; few, medium, faint, light brownish -gray (10YR 6/2) mottles and few, medium, distinct, brownish -yellow (10YR 6/6) mottles; weak, fine, subangular blocky structure; friable, slightly sticky and slightly plastic; few fine roots; thin, discon- tinuous clay films on faces of peds; very strongly acid; clear wavy boundary. B22tg 21 to 48 inches, gray (JOYR 6/1) sandy clay loam: common, medium, distinct, brownish -yellow QOYR 6/6). mottles; weak fne, subangular blocky struc- ture; friable, slighily sticky and slightly plastic; thin, discontinuous clay films on faces of peds; ve,y strongly acid; gradual, wavy boundary. B3g--48 to 66 inches, gray (10YR 6/1) sandy clay foam; common, medium, distinct andprominent, red (2.5YR 418) mottles; weak, fine, subangular blocky. os,.,,nt,,,.o. "Friable" s7ivhtly sticky and slightly Plas- Cg-66 to 85 inches, light -gray (10Ytt '1/1) sanuy c - y loam; few, medium, distinct, strong -brown (7.5YR 5/6) motiles and few, medium, faint, light brown- ish -gray (10yR 6/2) mottles- massive; friable, slightly sticky and slightly plastic; extremely acid. The solum is more than 60 inches thick. Reaction is strongly acid to extremely acid unless the soils are limed. The Al or Ap horizon is dark gray or dark grayish brown. The B horizon is pale brown or light yellowish brown and mottled with gray and yellow in the upper part. This hori- gon is sandy clay loam and to a lesser extent sandy loam. 18 SOIL SURVEY Below a. depth of. about. 21 inches it is gray and mottled with yellow and red. The C horizon is sandy loam or sandy clay loam. ILyilc➢nbur-9 sandy loam (Ly).—This soil is on broad, smooth flats of interstmam divides. Slopes are 0 to 2 percent. The areas are long and broad and range from 5 to about 100 acres in size. Included with this soil in mapping are areas of soils that have a surface layer of very fine sandy loam and loamy sand and some that have a siltier subsoil than this soil. .Also included are a few small areas of Goldsboro, Rains, and Stallings soils. Infiltration is moderate, and runoff is slow. Ifdrained, this soil is well suited to most focally grown crops, chiefly corn and soybeans. The principal tree species is loblolly pine. Surface and subsurface drainage is needed for most uses. The seasonal high water table is the main limitation in the use and management of this soil. Capability unit Hw-2; woodland suitability group 2w8. . The Meggett series consists of nearly level, poorly drained soil on uplands and stream terraces. In a representative profile the surface layer is darlt gray fine sandy loam about 8 inches thick. The sub- surface layer is light brownish -gray sandy loam about 4 inches thick. The subsoil is 33 inches thick. The up- per part is gray sandy clay loam that is mottled with yellow. The lower part is gray clay or sandy clay that is mottled with brown and yellow. Below the subsoil, to a depth of about 85 inches, is gray sandy clay Ioam that is mottled with yellow and gray. Meggett soils are medium in natural fertility and low in content of organic matter. Permeability is slow, and available water capacity is high. Shrink -swell po- tential is high. The seasonal high water table is at the surface. Most of the acreage is wooded. The rest is cultivated or pastured. ' Representative profile of Meggett_fine sandy loam in a cultivated field 8 miles east of Sinton, 0.1 mile south of the intersection of North Carolina Highway 55 and State Road 1806, 0.3 mile southwest of bridge on ditch road, and 50 feet west of ditch road. Ap—o to 8 inches, dark -gray (im 4/1) fine sandy loam; weak, medium, granular structure; very friable; common fine roots; medium acid; abrupt, smooth boundary. A2-8 to 12 inches, light brownish -gray (10YR 6/2) sandy loam; weak, medium, granular structure; very fri- able; common fine roots; common pores filled with dark gray; medium acid; clear, wavy boundary. B21t9-12 to 17 in gray (10YR 6/1) sandy clay loam; common, fiponne, angular black structure; friable, weak, medium, ky sticky and plastic, common fine roots; common pores filled with dark -gray sandy loam; slightly acid; gradual, wavy boundary. B22tg-77 to 30 inches, gray (10YR 5/1) clay; common, fine, distinct, strong -brown and yellowish -brown mottles; weak, coarse, angular blocky structure; firm, sticky and plastic; thin, discontinuous clay films on faces of peds and pores; few fine flakes of • lPigure 6—The ItIegget soils are underlain by marl an ramp mica; moderately alkaline; gradual, wavy bound- places. The marl shown above the waterline in this ditch is a ary. limitation to the installation of drau+age systems. B3g-30 to 45 inches, gray (rOYR 5/1). sandy clay; thin lenses of sandy Ioam and clay; common, medium, distinct, brownish -yellow (10 -YR 6/6) and yellow- ish -brown (1OYR 5/6) mottles; weak, medium, angular blocky structure; firm, sticky and plastic; few small fragments of marl; few fine flakes of mica; moderately alkaline; gradual, wavy boum- ary. Cg- 45 to 85 inches, gray (10YR 571) sandy clay loam; thin lenses of sandy loam and sandy clay; common, medium, distinct, brownish -yellow (10YR 6/8) and greenish -gray (5G 5/1) mottles; massive; friable; few small fragments of marl; moderately alkaline. The solum is 40 to 60 inches thick. Reaction is medium acid in the A horizon and the upper part of the B horizon to moderately alkaline in the lower part of the B horizon and the C horizon. The A horizon is very dark gray, dark gray, or grayish brown. where the surface layer is very dark gray, It is less than 8 inches thick. The B horizon is gray or light -gray clay, sandy clay, or sandy clay loam that is mottled with brown and yellow. The C horizon is sandy loaM, sandy clay loam, clay loam, or clay and in places con- tains fragments of friable to hard marl. llh[eggett �nso saaidly P®ammo (Me —This soil is in shal- low depressions on broad interstream areas and in drainageways. Slopes are 0 to 1 percent. The areas are long and narrow and range from 5 to about 50 acres in size. Included with this soil in mapping are a few areas of soils that have a surface layer of loam. Also included are a few small areas of Grifton, Lumbee, and Wood- ington soils. Infiltration and runoff are slow, and in places the surface becomes ponded. The soil is difficult to keep in good tilth, and, because of the moderately high clay content, it can be worked only over a narrow range of E content. If drained, this soil is well suited to a few locally grown crops, chiefly corn and soybeans. The trees are chiefly hardwoods and loblolly pine. Surface and sub- surface drainage is needed before this soil can be cul- tivated or pastured. In places, this soil is underlain by marl which, if hard, is a limitation in the construction of drainage ditches (fig. 6). L MOIR COUNTY, NORTH CAROLINA 'High shrink -swell potential, water ponding on the face, .and a'seasonal high water table are the main ,l nitations in the use and management of this soil. Capability unit IIIw-2; woodland' suitability group llw9. munrville sefles The Murville series consists of nearly level, very poorly drained soils on uplands. In a representative profile the surface layer is black fine sand about 7 inches thick. The subsoil is 51 inches thick. The upper part is very dark gray fine sand, the middle part is black fine sand, and the lower part is mottled, very dark gray and black fine sand. Below the subsoil, to a depth of about 87 inches, is gray loamy fine sand that is mottled with brown and black. The Murville soils are very low in natural fertility and medium in content of organic matter. Permeability is moderately rapid, and available water capacity is low. Shrink -swell potential is low. The seasonal high watei! table is at the surface. Most of the acreage is wooded. Representative profile of Murville fine sand in a wooded area east of the intersection of Stat Roads les south of Pink I1103 and ill and 01105 Al -0• to 7 inches, black (10YR 2/1) fine sand; weak, fine, granular structure; very friable; many large roots; grains o£ sandh in ; extreof mely acid;anic clear, wavy common bound- ary. ! Blh-7 to 20 inches, very dark gray (10YR 3/1) fine sand; massive; friable; many medium and large roots; many grains of clean sand, some slightly darker, slightly firm nodular bodies, extremely acid; clear, wavy boundary. B2h 20 to so inches, black (5YR 2/1) fine sand; massive; deanfriablsa de some lightly darker,w fine and slightly ots; fewfirm nodu- lar bodies; extremely acid; clear, wavy* 5YR 3 1 B3h-30 to 58 inches, mottled very dark gray ( / ) and black (5YR 2/1) fine sand that has common grains of clean sand, massive; friable; few me- dium and fine roots; some slightly darker, slightly firm nodular bodies; extremely acid; clear, wavy boundary. Cg -58 to 87 inches, gray (1oYR 6/1) loamy fine sand; common, coarse, distinct, very dark brown (10YR 2/2), dark reddish -brown (5YR 2/2), and black (5YR 2/1) mottles; massive; friable; extremely acid. The solum is about 40 to 50 inches thick. Reaction is ex- tremely acid or very strongly acid unless the soils are limed. The grains are coated with an organic film, and the soil has an apparent loamy texture to a depth of about 40 inches or more. The Bh horizon is very dark gray or black ers of humus fine ate grains of sad esand oil sand. In xtendelaces to pockets depth of more than 100 inches. Murville fine sand (Mu).—This soil is in depressions on broad, flat interstream areas. Slopes are less than 1 percent. The areas are mostly large and round, but some are irregularly shaped and small. small areas Included with this soil in mapping of Johnston, Leon, Pactolus, and ToThlmta soils. Infiltration is rapid, but water ponds on the surface. ' drained, this soil is suited to a few locally grown crops. If cultivated, corn and soybeans are the chief crops. The most important tree species are loblolly 79 pine, pond pine, loblolly bay, maple, sweet gum, and oak. Surface drainage and subsurface drainage are required if the soil is to be cultivated or pastured. Water ponding on the surface and a seasonal high water table are the main limitations in the use and management of this soil. Capability subclass IC7w, drained, and VIIw, undrained; woodland suitability group 2w9. Pt®rI011K offles The Norfolk series consists of nearly level to sloping, well -drained soils on uplands. In a representative profile the surface layer is gray- ish -brown loamy sand about 8 inches thick. The subsurface layer is pale -brown loamy sand about 4 inches thick. The subsoil is 60 inches, thick. The upper part is light yellowish -brown sandy loam. The middle part is yellowish -brown sandy clay loam that _is mottled below a depth of 45 inches with red and gray. The lower part is brownish -yellow sandy clay loam that is mottled with gray and red. Below the subsoil, to a depth of 85 inches, is gray sandy clay loam that is mottled with yellow and red. Norfolk soils are low in natural fertility and content of organic matter. Permeability is moderate, and avail- able water capacity is medium. Shrink -swell potential is low. The seasonal high water table remains at about 5 feet below the surface. Most of the acreage is cultivated. The rest is in non- farm uses. Representative profile of Norfolk -loamy sand, 0 to 2 P slopes, in a cultivated field 1.3 miles east of Newborn Crossroads, 0.4 mile south of intersection of State Road 1703 and State Road 1729, and 25 feet east of State Road 1729: Ap—o to 8 inches, grayish -brown (10YR 5/2) loamy sand; weak, medium, granular structure; very friable; common fine roots; strongly acid; abrupt, smooth boundary. .A2--8 to 12 inches, pale -brown (loYR 6/3) loamy sand; weak, medium, granular structure; very friable, common fine roots; strongly acid; clear, wavy boundary. B1=12 to 14 inches, light yellowish -brown (10YR 6/4) sandy loam; weak, fine, subangular blocky struc- ture; friable; common fine roots; very strongly acid, clear, wavy boundary. B211-14 to 5 inches, yeliowish-brown (10YR 5/8) sandy clay loam) weak, fine, subangular blocky structure; friable, +in�ssatlfissfio"dcntinuoudvlms on faces of to blocky structure; Enable, sugnviy suiexy anu s,�K„�+y plastic; thin, discontinuous clay films on faces of peds and pores; very strongly acid; gradual, wavy boundary. B3-60 to 72 inches, brownish -yellow (10YR 6/6) sandy clay loam; common, medium, distinct, light brown- ish -gray (loYR - 6/2) mottles and few, medium, prominent, red (2.5YR 4/8) mottles' weak, fine, subangular blocky structure; friable, slightly sticky and slightly plastic; very strongly acid; gradual, wavy boundary. C-72 to 85 inches, gray QoYR 6/1) sandy clay loam that has thin strata of sandy clay; common, medium, 20 SOIL .SURVEY 'distinct, brownish -yellow (IOYR 6/8) and red (2.5YR 4/8) mottles; massive; friable to firm.in sandy Clay strata; slightly sticky and plastic; very strongly acid. The solum is more than 60 inches thick. Reaction is very strongly acid or strongly acid unless the soils are limed. The Ali or Al horizon is grayish brown or light brownish gray. The, B horizon is light yellowish brown, yellowish brown, brownish yellow, or strong brown. The texture cen- ters on sandy clay loam, but in places the upper few inches is sandy loam. The lower part of the B horizon is mottled with gray and red. The C horizon is sandy loam or sandy clay loam that has thin strata'o£ sandy clay in places. yJgrfolk Iloaaaay wand, 0 to 2 gnerceant slopes (Na).— This soil is on smooth, broad, slightly convex. divides. The areas are irregularly shaped and range from 5 to about 200 acres in size. This soil has the profile de- scribed as representative for the series. fncluded.with this soil in mapping are a few areas of soils that have a surface layer of sandy loam and very fine sandy loam and some that have a siltier subsoil. Also included are a few small areas of Goldsboro and Wagram soils and a few. soils that have sandy clay sub- soils,. 40 to 60 inches below the surface. Some delinea- tions have a sand spot or one or more spots of wet soils in depressions. These spots of other kinds of soils Are shown in mapping by special spot symbols. Infiltration is moderate, and runoff is slow. This soil is well suited to most locally grown crops and is used chiefly for tobacco, corn, soybeans, truck crops, fruit crops, and small grain. It is especially well suited to tobacco. There are no major limitations in the use of this i soil. Capability unit I-1; woodland group 2ol. Norfolk loamy sand, 2 to 6 percent slopes (Nb).— This soil (fig. i) is on convex divides. The areas are long and narrow and range from 5 to 30 acres in size. Included with this soil in mapping are a few areas of soils that have a surface layer of yellowish -brown sandy Ioam and very fine sandy loam that is 4 to 3 inches thick and some that have a silty subsoil. Also included are a few small areas of Goldsboro and Wagram soils and a few areas of soils that have sandy clay 40 to 60 inches "below the surface. In places, mapped areas include short strips of Bibb soils in drainageways, a few small spots of a soil that is sandy throughout, and spots of wet soil in depressions_ Spe- cial symbols are used to show these spots. Infiltration is moderate, and runoff is. medium. and Craven soils: In places mapped areas include nar- This soil is well suited to most locally grown crops. raw strips of Bibb soils in drainageways. It is used chiefly for corn, tobacco, soybeans, truck Infiltration is moderate," and runoff is rapid. crops, and small grain and is especially well suited to This soil is well suited to most locally grown crops; tobacco. however, the short length and strong gradient of the Runoff is the main limitation in the use and man- slopes limit the use of this soil for row crops, agement of this soil. Capability unit IIe-1; woodland Slope and runoff are the main limitations in the group 201. use and management of this soil. Capability unit Norfolk loamy sawed, .6 to 10 pereent slopes (Nc).- Ille-1; woodland group 2ol. This soil is on short side slopes next to drainageways. The areas are long and narrow and range from 5 to 20 acres in size: Included with this soil in mapping are a few areas Th of soils that have a surface layer of sandy loam and 'very fine sandy loam that is 4 to 6 inches thick. Also t err included in mapping are a few small areas of Wagram Figare 7.—Pro81e of Norfolk loamy sand. e Pactolus series consists of nearly level, some- what poorly drained soils on uplands and stream aces, In a representative profile the surface layer is dark 24 SOIL . SURVEY a limitation to installation and maintenance of drain- age systems. Water ponding on the surface and a seasonal high water table are the main limitations in the use and management of this soil. Capability unit III _3, drained; capability subclass Vw, undrained; woodland Suitability group lw9. The Rains series consists of nearly level, poorly drained soils on uplands. In a representative profile the surface layer is dark - gray sandy loam about 10 inches thick. The subsurface layer is light brownish -gray sandy loam about 3 inches thick. The subsoil is about 72 inches thick. The upper part is light brownish -gray sandy clay loam, and the lower part is gray sandy clay loam' that is mottled r with brown and yellow. Rains soils are low in natural' fertility and content of organic matter. Permeability is moderate, and available water capacity is medium. Shrink -swell po- tential is low. The seasonal high water table is at the surface. Most of the acreage is wooded. The rest is cultivated and pastured. Representative profile of Rains sandy loam, in a cul- soutivth of the intersectionted field 0.4 of State Roae east 'of ds 541rand IB81t I e and 20 feet south of State Road 1581: Ap—O to 16 inches, dark -gray (1DYR 4/1) sandy loam; weak, medium, granular structure; very friable; many medium roots; medium acid; abrupt, smooth boundary. A2-10 to 13 inches, light brownish -gray (10YR 6/2) sandy loam* weak, medium, granular structure; very friable, many medium roots; common pores filled with dark -gray material from AP horizon; strongly acid; clear, wavy boundary. Blg-13 to 16 inches, light brownish -gray (10YR 6/2) sandy clay loam; weak, fine, subangular blocky structure; friable, slightly sticky and slightly plas- tic; few fine roots;.common pores filled with dark - gray material from AP horizon; very strongly acid; clear, wavy boundary. B21tg-16 to 34 inches, gray (10YR 6/1) sandy clay loam; common, medium, distinct, yellowish -brown (10YR 5/4) mottles; weak, fine, subangular bloeky struc- ture; friable, slightly sticky and slightly plastic; few fine roots., thin, discontinuous clay films on faces of peds; very strongly acid; gradual, wavy boundary. B22tg-34 to 48 inches, gray (YOYR 6/1) sandy clay loam; common, medium, distinct, yellowish -brown (10YR 5/4) and grayish -brown (loYR 5/2) mottles and few, fine, distinct, yellowish -red mottles; weak, fine, subangular blocky structure• friable, slightly sticky and slightly plastic; thin, discontinuous clay fibns on faces of Peds; very strongly acid; grad- ual wavy boundary. B23tg-48 to 63 inches, gray (10YR 6/1) sandy clay loam; few > medium, distinct, yellowish -brown (10YR 5/4) mottles and common, coarse, faint, grayish - brown (SoYR '5/2) mottles; weak, fine, subangular blocky 'structure; friable) slightly sticky and slightly plastic; very strongly acid; gradual, wavy. boundary. • Bsg-63 to 85 inches, gray UOYR 6/1) sandy clay loam that has thin lenses of sandy clay and sandy loam; few, coarse, faint, grayish -brown (10YR 5/2) and reddish-yellow (7.5YR 6/8) mottles; massive; friable, slightly sticky and slightly plastic; very strongly acid. The solum is more than 60 inches thick. Reaction is strongly acid or very strongly acid unless the soils are limed. The Al or Ap horizon is dark gray or very dark gray. Where the surface layer is very dark gray, it is less than 8 inches thick. The B horizon is gray or light -gray" sandy clay loam and, to a lesser extent, sandy loam that is mottled' with brown, yellow, and red. Rains sandy loam (Ra)'.—This soil is in depressions and on smooth flats in broad interstieam areas. Slopes are less than I percent. The areas are generally long and wide and range from 5 to several hundred acres in size. Included with this soil in mapping are a few areas of soils that have a surface layer of loam and very fine sandy loam and some that have a siltier subsoil. Also included are a few small areas of Coxville, Lynch- burg, and Pantego soils. Infiltration is moderate, and runoff is slow or the surface is ponded. If drained, this soil is well suited to a few locally grown crops, chiefly corn and soybeans. The principal tree species is loblolly pine. Surface' and subsurface drainage is needed before this soil can be cultivated or pastured. Water ponding on the surface and a seasonal high water table are the main limitations in the use and management of this soil. Capability unit IIIw-3, drained• capability subclass Vw, undrained; woodland suitab8y group 2w3. ��et.H�flIlfl�'3 The Stallings series consists of nearly level, some- what poorly drained soils on uplands and stream Terraces. In a representative profile the surface layer is dark - gray loamy sand about 8 inches thick. The subsurface layer is light brownish -gray loamy sand about 4 inches thick. The subsoil is 68 inches thick. The upper part is pale -brown sandy loam that is mottled with gray and brown, the middle part is light -gray sandy loam that is mottled with brown and yellow, and the lower part is light brownish -gray loamy sand that is mot - tied with gray and brown. Stallings soils are low in natural fertility and con- tent of organic matter. Permeability is moderately rapid, and available water capacity is medium. Shrink - swell potential is low. The seasonal high water table is within 15 inches of the surface. About half the acreage is cultivated. A small acreage is in pasture, and the rest is wooded. Representative profile of Stallings loamy sand in a cultivated field 8 miles south of Kinston, 0.5 mile south of Woodington on U.S. Highway 258, and goo feet east of U.S. Highway 258: Ap—O to 8 inches, dark -gray (10YR 4/1) loamy sand; weak, medium, granular structure; very :friable; many fi ne roots; strongly acid; abrupt, smooth boundary. A2-8 to 12 inches light brownishBy(JOYR 6/2) loamy sand; weak, medium, granular structure; very fri- able; many fine roots; strongly acid; clear, Wavy boundary. i" V�TH SOIL SURVEY Umbrie Oehraqualfs are low in natural fertility and medium in content of organic matter. Permeability is moderate, and available water capacity is medium. Shrink -swell potential is moderate. The seasonal high water table is at the surface. Most. of the,acreage is wooded. The rest is cultivated and pastured. Representative profile. of Umbrie Oehraqualfs, 0.3 mile south of Loftin's Crossroad, 0.3 mile east of the intersection of North Carolina Highway 58 and State Road 1914, and 100 feet south of State Road 1914: Ap-0 to 11 inches, black (10YR 2/Y) loam; weak, medium, granular structure; friable; common medium roots; strongly acid;. gradual, wavy b lOYR 3/1) loam; AZ -11 to 14 inches, very dark gray weak, medium, granular structure; friable; com- mon medium roots; common pores filled with black surface soil; strongly acid; gradual, wavy bound- ary. Blg-14 to 18 inches, grayish -brown (lOYR 5/2) sandy ' clay loam; weak, fine, subangular blocky structure; friable; common fine roots; £ew pores filled with black loam; strongly acid; gradual, wavy bound- ary.. B21tg-11 9 loam Cheommony1 medium, distinet,5 yeIlovrish ' bxown (lOYR-5/6) mtittle5, weak fine, subangular blocky structure; friable, slightly sticky and slightly plastic; thin, discontinuous clay films on faces of peds and pores; medium acid; gradual, wavy boundary. B22tg-34 to 42 inches, gray (lOYR 6/1) sandy clay that has thin strata of sandy loam; few, medium, dis- tinct, yellowish-brown'(lOYR 5/6) mottles; weak, fine, subangular blocky structure• friable, slightly sticky and slightly plastic; thin, discontinuous clay Elms on faces o£ peds and pores; neutral; gradual, wavy boundary. �B3g-2 to 70� inches, gray �(IOYR 6/1) sandy clay loam that has thin strata of sand and greenish -gray clay; massive; friable, slightly sticky and slightly plastic; mildly alkaline. The solum is more than 6D inches thick. Reaction is strongly acid in the A�horizon and BY horizon unless the soils are limed and medium acid to mildly alkalinein the lower part o£ the B horizon. The A horizon is black or very dark gray. The B horizon is grayish -brown or gray sandy clay loam or sandy clay that is mottled with bxovm and gray. The underlying horizons are soft marl mixed with loamy sand, sandy clay loam, or clay. VJan6ric ®chraqualfs (Uo).—This soil is on broad, smooth flats' on interstream areas. Slopes are less than 1 percent. The areas are wide and long and range from 20 to about 15D acres in size. Included with this soil in mapping are a few small areas of Grifton, Meggett, Portsmouth, and Torhunta SOILS. Infiltration is moderate. Runoff is very slow or the surface is ponded.' If drained, this soil is well suited to a few locally grown crops, chiefly corn and soybeans. The important tree species are loblolly and pond pine. Surface and subsurface drainage is needed before this soil can be cultivated or pastured. In pIaees this soil is underlain by marl, which may present a problem to construction of ditches. VJatei ponding on the surface and a seasonal high water table are the main )imitations in the use and. management of these soils. Capability unit I7Iw-3; woodland suitability group 1w9. � �i:�iii ,•�i�ir The pPag'ram series consists of nearly level to strongly sloping, well -drained soils on uplands. In a representative profile the surface layer is grayish -brown loamy sand about 8 inches thick. The subsurface layer is pale -brown loamy sand about 22 inches thick. The subsoil is sandy clay loam 51 inches thick. The upper part is yellowish brown, the middle part is brownish yollow.,mottled with red and gray, and the lower part is light yellowish brown mottled with brown and gray. Below the subsoil, to a depth of 9D inches, is brownish -yellow sandy clay loam that is mottled with brown and red. Wagram soils are low to very low in natural fer- tility and content of organic matter. Permeability is moderately rapid, and available water capacity is low. Shrink -swell potential is low. The seasonal high water table remains below a depth of about 5 feet. Most of the acreage is cultivated. The rest is used for nonfarm purposes. Repxesentative profile of �agram loamy sand, 0 to 6 percent slopes, in a cultivated field 2.4 miles south- east of LaGrange, 0.4 mile southeast of intersection of U.S. Highway 70 and State Road 1520; and 20 feet east of farm road: Ap-0 to 8 inches, grayish -brown (lOYR 5/2) loamy sand; weak, medium, granular structure; very friable• common fine roots; medium acid; abrupt, smooth boundary. A2-8 to 30 inches, pale -brown (lOYR 6/3) loamy sand; common, medium, faint mottles of uncoated sand; weak, medium, granular structure; very friable; few fine roots; very strongly acid; gradual, wavy boundary. B21t-3D to 58 inches, yellowish -brown (IOYR 5/8) sandy clap loam; weak, fine; subangular blocky structure; .friable, slightly sticky and slightly plastic; thin, discontinuous clay films on faces of peds; very strongly acid; gradual, wavy boundary. B22t--58 to 71 inches, brownish -yellow (lOYR 6/8) sandy clay loam• common, medium, prominent, red (2.5YR 4/8) mottles and few, medium, distinct, gray (lOYR 6I1) mottles; weak fine, subangular blocky structure• £ruble, slightly sticky and slightly plastic; thin, discontinuous clay films on ' faces of peds; very strongly acid; gradual, wavy boundary. - B3-71 to 81 inches, light yellowish -brown (lO�YR 6/4) . " � sandy clay loam; common, medium, distinct, strong- ' brown (7.5YR 5/8) and gray (lOYR 6/Y) mottles; weak, -fine, subangular blocky structure; friable, slightly sticky and slightly plastic; very strongly acid; gradual, wavy boundary. C-81 to 90 inches, brownish -yellow (IOYR 6/6) sandy clay loam• common, coarse, distinct, gray (1-0YR 6/1) mottles and common, fine, distinct, strong - brown mottles and common, fine, prominent, red mottles; massive; very friable, slightly sticky and slightly plastic; very strongly acid. The solum is more than 60 inches thick. Reaction is strongly acid or very strongly acid unless the soils are limed. The Ap or AY horizon is grayish brown or light grayish brown: "The B horizon is light yellowish -brown, yel- lowish -brown, brownish -yellow, ox strong -brown sandy clay loam or sandy loam that is mottled with red, brown, and gray in the lower part. The C horizon is sandy clay loam, sandy loam,. or loamy sand. OPagraau floamy sand, 0 to 6 percent slogoes (Wb)� - his soil is on slightly convex divides. The areas are regularly shaped and range from 10 to about 50 LENOIR COUNTY, NORTH CAROLINA acres in size. This soil has the profile described as -esenta'tive for the serieso ncluded with Eris soil in mapping are a few areas of soils that have a surface layer of sand. Also in eluded are a few small areas of Blanton, Goldsboro, Norfolk, and Pocalla soils. Short, narrow strips of Bibb soils in `drainageways and -a few, small depres- sions of wet soils are also included. Those wet soils are shown by wet spot symbols. Infiltration is moderate, and runoff is slow. This soil is suited to most locally grown crops and is used chiefly for tobacco, corn, soybeans, and small grain. Leaching of plant nutrients, low available water capacity, and the hazard of soil blowing ate the main limitations in the use and management of this soil. Capability unit II8-1; woodland suitability group 3s2. Wagram loamy saBd, 6 to 110 percent sl®pes (Wo); This soil (fig. 9) is next to drainageways where side slopes are short. The areas are long and narrow and range from 5 to 100 acres in size. Included with this soil in,mapping are a few areas of soils that have a surface layer of sand. Also in - Fig¢re 9.—ProSle of Wagram Ioamy sand. 27 chided are a few small areas of Blanton, Craven, and Norfollc soils. Narrow strips of Bibb soils in drainage - ways are also included. Infiltration is moderate, and runoff is medium. This soil is fairly well suited to most locally grown crops, but the short length and gradient of the slopes limit the use: of this soil for row crop.,,cultivation. Run- off causes a hazard of erosion if this soil is cultivated. Leaching of plant nutrients, low available water capacity, runoff, and slope are the main limitations in the use and management of this soil.. Capability sub- class IIIs; woodland suitability group 8s2. Wagrwn loamy salad, 10 to 15 pexeent sloPes (Wd) .— Th s soil is between gently sloping uplands and flood plains or stream terraces. The areas4 are long and narrow and range from 5 to 75 acres in size. Included with this soil in mapping are a fewsmall areas of soil that has steeper slopes and areas of soil that has a surface layer of sandy loam. Also included are a few small areas of Bibb, Blanton, Craven, and Lakeland soils. Infiltration is moderate, and runoff is rapid. This soil is fairly well suited to most locally grown crops, but the short length and gradient of the slopes limit the use of this soil for row -crop cultivation. Run- off causes a hazard of erosion if this soil is cultivated. Practices are needed to control runoff and erosion. Leaching of plant .nutrients, low available water capacity, runoff, and slope are the main limitations in the use and management of this soil. Capability sub- class IVs; woodland suitability group 3s2. The Wickham series consists of nearly level to gently sloping, well -drained soils on stream terraces. In a representative profile the surface layer is brown loamy sand about 8 inches thick. The subsurface layer is light yellowish -brown loamy sand about 7 inches thiek. The subsoil is 28 inches thick. The upper part is strong -brown sandy clay loam, the middle part is yellowish -red sandy clay loam that is mottled .with brown, , and the lower part is strong -brown sandy loam. Below the subsoil, to a depth of 65 inches, is brownish -yellow Ioamy sand. Wickham soils are low in natural fertility and con- tent of organic matter. Permeability is moderate, and available water capacity is medium. Shrink -swell po- tential is low. The seasonal high water table remains below a depth of 5 feet. Most of the acreage is cultivated. The' rest is pas- tured. Representative profile of Wickham loamy sand, 1 to 6 percent slopes, m i cultivated field,5.7 miles south Roe west of intersection of State ads 100 LaGranBand 1313, and 25 feet northof State Road 1313: Ap-0 to 8 inches, brown UOYR 613) loamy sand; weak, medium, granular structure; very friablesm- mon fine roots; medium acid; abrupt,mo th boundary. 10YR 61 4) A8-8 to 16 inches, light yellowish-bro�r structure; friable; sand; weak, medium, graniila very common fine roots; strongly acid; abrupt, wavy boundary. 28 SOIL SURVEY B1-15 to 19 inches, strong -brown (7.5YR 5/6) sandy clay loam; weak, fine, subangular blocky structure; fri- able; common ri- able;'common fine roots; strongly acid; clear, wavy boundary. B21t-19 •to 25 inches, yellowish -red (5YR 4/8) sandy clay loam; moderate, fine, subangular blocky structure; friable, sticky and plastic; clay films on .faces of `peds; few flakes of. mica and feldspar grains; strongly acid; gradual, wavy boundary. B22t-25 to 38 inches, yellowish -red (5YR 5/8) sandy clay loam; few, medium, faint, yellowish -brown (10YR 5/4) mottles; weak, fine, subangular blocky strue- ture, friable, slightly sticky and slightly plastic; common small flakes of mica and few feldspar grains; strongly acid; gradual, wavy boundary. B3-38 to 43 inches, strong -brown (7.5YR 5/8) sandy loam; weak, fine, subangular blocky structure; very friable; common small flakes of mica; strongly acid; gradual, wavy boundary. — IIC43 to 65 inches, brownish -yellow (lOYR 6/6) loamy sand; single grained; very friable; common small flakes of mica and few feldspar grains; few peb- bles; strongly acid. The solum is about 40- to 55 inches thick. Reaction is strongly acid to slightly acid unless the soils are limed. The Ap and Al horizons are brown or grayish brown, and the A2 horizon is light yellowish brown oriole brown. The B horizon is yellowish -red or strong -brown clay loon, sandy - clay loam, or sandy Ioam that is mottled with brown in the . lower part. The C horizon is loamy sand'or sand and gen- erally contains gravel: Wickham loamy nand, 1 to 6 percent nH®g¢s ( Wk): This soil is on smooth, low ridges. The areas ai longer than they are wide and range from 5 to acres in size. Included with this soil in mapping are a few aree of eroded soils that have a surface layer of yellowish brown sandy loam and loam. Also included are a fe, small areas of Kahmia and Kenansville soils. Strip of Bibb soils in. drainageways and a few small spot of deep sand or wet spots are also included. Thes wet spots are shown in mapping by special spot sym bots. Infiltration is moderate, and runoff is medium. This soil is well suited to most locally grown crops It is used chiefly for corn, tobacco, soybeans, and small grain. Runoff is the main limitation in the use and man agement of this soil. Capability unit IIe-1; woodland Suitability group 2o7. The Woodisigton series consists of nearly level,_ _poorly drained soils on uplands and stream terraces., In a representative profile the surface layer is very dark gray loamy sand about 4 inches thick.. The sub- surface layer is grayish -brown loamy sand about 8 inches thick. The subsoil is 73 inches thick. The upper part is light brownish -gray sandy loam that is mottled with brown, the middle part is gray sandy loam that is mottled with brown and gray, and the lower part is light -gray loamy sand that is mottled with yellow. Woodington soils are low in natural fertility and content of organic matter. Permeability is moderately rapid, and available water capacity is medium. Shrink - swell potential is low. The seasonal high water table s within 12 inches of'the surface. Most of the acreage is wooded. The rest is cultivate( and pastured. Representative profile of Woodington loamy sand u a wooded area 5 miles south of Kinston, 0.5 mile nortl of the intersection of State Roads 1161 and 1149, anc 10 feet north of State Road 1149: Al -0 to 4 inches, very dark gray (10YR 3/1) loamy sand; weak, medium, granular strtieture; very friable; many. fine roots; very strongly acid; gradual, wavy boundary. A2-4 to 12 inches, grayish -brown (10YR 5/2) loamy sand; weak, 'medium, granular structure; very -friable- many fine roots; few medium pores filled with dark -gray material from the surface layer; very strongly acid; clear, wavy boundary. B21tg-12 to 16 inches, light brownish -gray (10YR 6/2) sandy Ioam; few., medium, distinct, light yellowish - brown (10YR 6/4) mottles; weak, fine, subangular blocky structure; very friable; slightly sticky; sand coated and bridged with clay; few medium pores filled with dark -gray material from the surface layer; very strongly acid; gradual, wavy boundary. B22tg-16 to 32 inches, gray (10YR 611) sandy loam; few, medium, distinct, light yellowish -brown (10YR 6/4) and strong"brown (7.5YR 5/6) mottles; weak, fine, .subangular blocky structure; friable; slightly sticky; sand coated and bridged with clay; very strongly acid; gradual, wavy boundary. B23tg--32 to 47 inches, gray (10YR 6/1) sandy loam; com- mon pockets of light -gray (10YR 7/1)'and yellow- ish -brown (10YR 5/4) sand; weak, fine, subangular blocky structure; very friable; very strongly acid; gradual, wavy boundary. - B3g=47 to 86 inches, light -gray '(10YR. 7/1) loamy sand; few, medium, distinct, brownish -yellow (IOYR 6/6) mottles; weak, fine, granular structure; Ioose; com- mon small bodies of clean sand; very strbngly acid. The solum is more than 60 inches thick. Reaction is very strongly acid or strongly acid unless the soils are limed. The Ap or Al horizon is dark gray or very dark gray. The very dark gray surface layer is less than 8 inches thick. The.B horizon is gray or light brownish gray and is mottled with yellow and brown. The upper part is sandy loam, and the lower part is loamy sand or sandy loam. The C horizon is sandy loam or loamy sand. Woodistg2on loamy sand ( Wn),—This soil is on broad, smpoth flats on interstream areas and in depressions. _ Slopes are less than 1 percent. The areas are about as. wide as they are long and range from 10 to 50 acres in size. Included with this soil in mapping are a few areas of soils that have a surface layer of fine sandy loam. Also included are a few small areas of Lumbee, Rains, Stallings, and Torhunta soils and small areas of soils that have an intermittent, thin layer of hardpan and concretions at a depth of 4 to 6 inches. Infiltration is moderate, and runoff is slow to'ponded. If drained, this soil is well suited to a few locally grown crops, chiefly corn and soybeans. The important tree species is loblolly pine. Surface and subsurface drainage is needed if this soil is cultivated'or pastured. Where the Iower part of the subsoil is sandy, there is z in in ditchbanks. This is a limitation in drain- age installation and maintenance. Runoff and a seasonal high water table are the main limitations . in the use and management of this soil. Capability unit IIIw-3, drained; capability subclass VIw, undrained; woodland suitability group 2w9. 32 SOIL SURVEY TABLE 2. -Estimated average acre yields of crops under intensive management Absence of yield means that the crop is not commonly grown on the soil or that yield estimates are not available] 'AUX stands for animal -unit -month. This is a term used w expEGbb su_-__-- months 1 acre will support one animal unit, such as one cow, one steer, one horse, fi Corn Soybeans Tobacco Cucum- bers Sweet- potatoes Wheat Coastal bermuda Pasture Fescue Coastal Soil hay and ber- clover muda Lb Bu Bu Bu Tons AUMV AUM% Bss Bu. 8'0 Bibb soils, frequently flooded -------------poop-- 10 160 35 25 1,600 _-- _ 55 3.5 slopes ____---____ Blanton sand, O'fr .: ___ - ___ 740 ___ qumtlent ChewacIa loam, frequently flooded _______ 90 40 ___ 45 --- 7.0 --- Coxville loam --------- -- '------ ----------- 85 105 40 2,560 --- --- 56' 6.0 7.0 --- raven fine sandy loam, 1 to 4 percent slopes ------ ___ 5.0 6.5 -- Craven fine sandy loam, 4 to 8 percent slopes ------ -46 -- 290 3b0 66 6.D Coldsboro loamy, sand, 0 to 2 percent slopes -------- 114 40 3,000 9.0 3rifton sandy loam ------------ --------- --poop-- 45 -- 2,760 -- 270. ___ 50 5.0 8,0 1 .0 120 6.0 fohns sandy loam --------- --------------------- 80 40 ' fohnston sods -- - ------ ------------- - - 110 45 2,906 225 300 60 5.5 '• �ahnia loamy sand, 0 to 2 percent slopes --------- 40 2,800 220 _ 55 5.0 ialmia loamy sand, 2 to 6 percent slopes ---poop-- 100 30 2,00 300 45 4.5 9.D Cepansville loamy sand, 0 to 6.percent slopes ___- 70 --- Citiston loam, frequently flooded ____-__-- ' --- --- 20 --- -- --- 3.D� ___ 6.0 .akeland sand, 6 to 6 percent slopes --------poop-- 55 35 -- --- -- _-- --- &0 --- 100 -- -- 8.0 ,eaf loam poop ------poop----------------- 95 45 2,206 --- --- --- ,enoir loam --------------'---- ______________ -- 3.0 --- 7.0 ,eon sand ---------------------poop-- 116 45 -- -,5 --- 1140 ,umbee sandy loam -----------------------poop---' 110 46 2,6-- 5.5 7.0 ynehburg sandy loam -------------------------- Y10 40 --- --- _-- --- 8.0 _-- 4eggett fine sandy loam ------------------------ Zurville.fine sand _____-- ----------- 126 40 3,000 29D 370 60 6.0 _ 10.5. orfolk loamy sand, 6 to 2 percent slopes --poop-- 2,96D 280 350 55 6.0 7.5 10.5 loamy 2 to 6 percent slopes ______-- 115 35 50 5.5 7.0 IDA (orfolk sand, forfolk loamy sand, 6 to 10 percentslopes ---poop -70 30 --- -- --- 3.4 'actolus-loamy sand -----------------------poop- 90 40 .1,800 --- -- --- _-- --- --- amlico muck --------� ----------poop--------- 50 --- --- -- --- --- antego loam ---_-----poop--en - opes--------- .110 30 2,000 300 40 5.D . 9.00 7. 0 to 6 percent slopes ---poop=- 80" ___ walla loamy sand, 110 40 --- --- ortsmouth loam -------- --poop------poop-- ----- 110 40 2,200 --- -- 8.0 -- - nine sandy loam ...... -------- ---------------- 105 40 2,560 -- ___ __- 4.8 SA 11.5 tallings loamy sand -_---------.----------- ___ 90 30 --- -- --- . --- 8.0 -'- orhunta loam - ----poop--pooppooppoop--poop-- 100 3D --- 9.0 mbrie Ochraqualfs ------------- ----------- 80 30 2,400 ___ 300 40 6 9.0 8,15 agram loamy sand, 0 to S percent slopes -------- 20 2,100 7.5 --- 'agram loamy sand, 6 to 16 percent slopes -poop-- 70 _-- --- 60 6.5 'agram loamy sand, YO to 15 percent slopes ------ - 356 6.0 10•5 'ickham 1 to 6 slopes _____-- 165 40 2,000 225 _-- 9.5 0 loamy sand, percent 110 40 --- --- 'oodington loamy sand ___________ ------------- --- --- ..;+., ,.s ., „n�,,,•P i+ 9e the number of ve hogs, or seven sheep or goats without dam - ate to the sod, no significant restrictions or limitations for woodland The management problems evaluated in the three use or management. The Hurd element in the symbol indicates the degree of management problems and the general suitability of the soils for certain kinds of trees. In the second column is a brief description of the soils in the woodland suitability group. In the third column is a list of some of the commer- cially important trees that are suited to the soils in the group. These are the trees that woodland managers Will, generally favor in intermediate or improvement cuttings. In column 4 the potential productivity of these trees is given in terms of site index. The site index is the average height of dominant trees, in feet, at age 30 for cottonwood; at age 35 for sycamore; and at age 50 for all other species or types. Listed in columns 5 and 6 are commercial broad- leaved and needle -leaved trees suitable for planting in soils of each group* columns at the.far right of table 3 are erosion hazard, equipment limitations, and seedling mortality. Erosion hazard measures the risk of soil losses in well-managed woodland. Erosion hazard is slight if expected soil loss is small, moderate if some measures to control erosion are needed in logging and construction, and severe if intensive treatment or special equipment and methods are needed to prevent excessive soil losses. Equipment limitation ratings reflect 'the soil con - ons that restrict the use of equipment normally used in woodland management or harvesting. Slight ratings indicate equipment use is not limited to Idnd or time of year. A rating of moderate indicates a seasonal H or need -for modification in methods or equip- ment. Severe limitations indicate the need for special- ized equipment or operations. Seedling mortality ratings indicate the degree of ex- pected mortality of planted seedlings where plant com- LENOIR COUNTY, NORTH CAROLINA 33 petition is not a limiting factor. Normal rainfall, good 25 percent, a moderate rating indicates a loss of 25 to .ting stock, and proper planting are assumed. A 50 percent, and a severe rating indicates a loss of more s .ght rating indicates expected mortality is less than than 50 percent of the seedlings. TABLE 3.—Potential productivity, preferred species of trees, and hazards to management, by woodland suita- bility groups of soils' Woodland suitability Description of soils groups, soil series, in group and map symbols Group 1w8: Chewacla: Ch. Group Iw9: Johnston: JS. ]Kinston: Kn. Meggett: Me, Pantego: Pe. Portsmouth: Pi Umbria Ochraqualfs: Uo. Group 201: Nor£ollc: Na, Nb, Na, Group 207: galmia: Ka, Kb. Wickham: Wk Nearly level, some- what poorly drained soils that have a loamy subsoil; on flood plains, subject to frequent flood - Nearly level, paorl drained or very poorly drained soils that have a loamy or clayey subsoil; on flood plains, stream terraces, and up- lands; subject to veryfrequent flooding; very high potential productivity; suitable for needle -leaved trees, broad- leaved'trees, or a combination of both. Nearly level to slop- ing, well -drained soils that have a loamy subsoil; on uplands; high po- tential productiv- jty; no serious management problems; best suited to needle - leaved trees. Nearly level - and gently sloping, . well -drained sods that have a loamy subsoil; on stream terraces; high potential productivity; no serious man- agement prob- lems • suited to needle -leaved trees, broad- leaved trees, or a combination of both. Trees pxeferi ed for Potential productivity management and planting Trees Loblolly pine _ Slash pine ___ Sweetgum Yellow -poplar Water oak ___ Wi1Iow oak _ _ _ Cherrybark oak. Cottonwood Green ash Sycamore Sweetgum' _-- Water oak' _-- Willow oak'_ Loblolly pine Slash pine' Cottonwood' _ Loblolly pine . Slash pine _ _ __ Longleaf pine Loblolly pine Slash pine _ _ _. Longleaf pine Yellow -poplar Sweetgum 114 90 90 Y00 100 100 Sweetgum', green ash' yellow -pop- lar', willow oak', water oak', white oak', swam; chestnut oak',syca- more ', swamp tupelo. Loblolly pine as pine' and pine'! bald- cypress. 90 Soils not suit- Loblolly pine, 90able. slash pine, 70 longleaf pine. 90 90 70 100 90 Yellow -pop - lar, sweet - heriybark oak, shumaid oak, south- ernred oak, wh to oak, black walnut, white ash. Loblolly pine, slash pine, Erosion ]quipment Seedling hazard limitations I mortality __� Moderate Slight __I Severe' __. Mod- erate. � Severe.' ISIight__� Slight ____� Slight. Siight __I Slight ____� Slight. d -leaved Needle-Ieaved ecies speciesrn • Loblolly pine,tonwood, slash pine,etgurn, bald - en ash, eypress.mard,rrybark,amore,ow-pop- PtUPB10. swampelo. 114 90 90 Y00 100 100 Sweetgum', green ash' yellow -pop- lar', willow oak', water oak', white oak', swam; chestnut oak',syca- more ', swamp tupelo. Loblolly pine as pine' and pine'! bald- cypress. 90 Soils not suit- Loblolly pine, 90able. slash pine, 70 longleaf pine. 90 90 70 100 90 Yellow -pop - lar, sweet - heriybark oak, shumaid oak, south- ernred oak, wh to oak, black walnut, white ash. Loblolly pine, slash pine, Erosion ]quipment Seedling hazard limitations I mortality __� Moderate Slight __I Severe' __. Mod- erate. � Severe.' ISIight__� Slight ____� Slight. Siight __I Slight ____� Slight. 34 SOIL SURVEY H TABLE S.—Potential productivity; preferred species of trees, and hazards to management, by woodland suita bility groups of soils—Continued Trees preferred for Woodland Potential productivity management and planting suitability Description of soils Erosion Equipment Seedling groups, soil series, in group Trees Site Broad-leaved Needle -leaved hazard limitations mortality and map symbols class' species species - Group 2w2: Nearly level, mod- Loblolly pine _ _ 90 None recom- Loblolly pine, Slight . _ Moderate _ Mod - Johns: Jo. .erately well Slash pine __ 90 mended. slash pine, erate. _ drained or some- Longleaf pine - 70 longleaf- what poorly pine. Group 2w3: Rains: Ra. Group 2w8: Goldsboro: Go Lenoir: Ln_ Lynchburg: Ly. Stallings: St. Group 2w9: Bibb: BB. Coxvi m: Co, Griftont Gr. Leaf: Le. Lumbee: Lu. Murville: Mu. Torhunta: To. Woodington: Wn. Group 3s2: Blanton: Bn. %enansville: Ke. Pocalla: Po. Wagram: Wb, We, Wd. drained soils tb have a loamy subsoil; high pr tential produc- tivity; best suit to needle-leavec trees. Nearly level, poor: drained soils the have a loamy subsoil; ubsoil • on up- lands; high po- tential pro- ductivity; best suited to needle - leaved trees. Nearly level, mod- erately well drained or some- whatpoorly drained soils tha have a loamy, clayey or sandy subsoil; on up - lauds and stream terraces; high po- tential produc- tivity; suited to needleleaved trees, broadleaved trees, or a com- bination of both. Nearly level, poorly drained or very poorly drained soils that have a loamy, sandy or clayey subsoil; on flood plains, up- lands and stream terraces' high potential produe- tivity; salted to broad-leaved trees, needle - leaved trees, or a combination of both. Nbarly level to strongly sloping, well drained or somewhat exces- sively drained soils that have a loamy or sandy subsoil; on up- lands and stream terraces moder- ately high potential pro- ductivity; best suited to ueedie- leaved trees. dI P I Loblolly pine' C Slash pine' __ Longleaf pine' Sweetgum' Loblolly pine _ _ Slash pine ____ Longl'ea£ pine _ Sweetgum --- Water oak _ Yellow -poplar . Loblolly pine' - Slash Sweetgum' Water oak' Willow oak' Green ash' Cottonwood 90 90 90 90 90 90 100 Loblolly pile 80 flash Longleaf pine _ 70 l None recom- mended. Sweetgum, yellow -pop- lar, water oak, willow oak, white oak, swamp chestnut oak, cherrybark oak. Sweetgum', yellow -pop- lar' willow oak 1, water oak',- cherrybark oak', oh oar oak', green ash', sycamore', swamp tupelo. Loblolly pin slash pine pine. Loblolly pine' slash pine', longleaf pine.', bald - cypress. 1',I Slight _-ISevere'_. .I Moderate (Severe'___ _ I Severe'. ISlight to mod- erate. Severe'. tTone recom- Slash pine, Slight _ _ Moderate _ Mod - mended. loblolly crate. pine, long- leaf pine. Group 2w3: Rains: Ra. Group 2w8: Goldsboro: Go Lenoir: Ln_ Lynchburg: Ly. Stallings: St. Group 2w9: Bibb: BB. Coxvi m: Co, Griftont Gr. Leaf: Le. Lumbee: Lu. Murville: Mu. Torhunta: To. Woodington: Wn. Group 3s2: Blanton: Bn. %enansville: Ke. Pocalla: Po. Wagram: Wb, We, Wd. drained soils tb have a loamy subsoil; high pr tential produc- tivity; best suit to needle-leavec trees. Nearly level, poor: drained soils the have a loamy subsoil; ubsoil • on up- lands; high po- tential pro- ductivity; best suited to needle - leaved trees. Nearly level, mod- erately well drained or some- whatpoorly drained soils tha have a loamy, clayey or sandy subsoil; on up - lauds and stream terraces; high po- tential produc- tivity; suited to needleleaved trees, broadleaved trees, or a com- bination of both. Nearly level, poorly drained or very poorly drained soils that have a loamy, sandy or clayey subsoil; on flood plains, up- lands and stream terraces' high potential produe- tivity; salted to broad-leaved trees, needle - leaved trees, or a combination of both. Nbarly level to strongly sloping, well drained or somewhat exces- sively drained soils that have a loamy or sandy subsoil; on up- lands and stream terraces moder- ately high potential pro- ductivity; best suited to ueedie- leaved trees. dI P I Loblolly pine' C Slash pine' __ Longleaf pine' Sweetgum' Loblolly pine _ _ Slash pine ____ Longl'ea£ pine _ Sweetgum --- Water oak _ Yellow -poplar . Loblolly pine' - Slash Sweetgum' Water oak' Willow oak' Green ash' Cottonwood 90 90 90 90 90 90 100 Loblolly pile 80 flash Longleaf pine _ 70 l None recom- mended. Sweetgum, yellow -pop- lar, water oak, willow oak, white oak, swamp chestnut oak, cherrybark oak. Sweetgum', yellow -pop- lar' willow oak 1, water oak',- cherrybark oak', oh oar oak', green ash', sycamore', swamp tupelo. Loblolly pin slash pine pine. Loblolly pine' slash pine', longleaf pine.', bald - cypress. 1',I Slight _-ISevere'_. .I Moderate (Severe'___ _ I Severe'. ISlight to mod- erate. Severe'. tTone recom- Slash pine, Slight _ _ Moderate _ Mod - mended. loblolly crate. pine, long- leaf pine. LENOIR COUNTY, NORTH CAROLINA "ABLE 3.—Potential productivity, preferred species of trees, and hazards to management, by woodland suita-bility groups of soils—Continued Trees preferred for Woodland Potential productivity management and planting Erosion Equipment Seedling suitability Description of soils groups, soil series, in group Trees Site Broad-leaved Needle -leaved hazard limitations mortality and map symbols - class' species species- Group3w2: Nearly level to slop- Slash pine ___ 80 None recom= SIash pine, Slight __ Moderate _ Slight, Craven: Cr, Cv, ing, mainlymod- Loblolly pine _ 80 mended, loblolly Pactolus: Pa, erately well Longleaf pine _ 70. _ pine,long- drained soils that leaf pine. have a loamy or clayey subsoil; on uplands and stream terraces; moderately high potential prodne- tivity; best suited to needle -leaved trees. Group 4s2: Lalceland: -a. G'^nup 4w2: :osl: Lo. 'Group 4w3: Pamlico: Pc. Nearly level to gently sloping, excessively drained soils that have a sandy underlying layer; on uplands and stream terraces; moderate pohm- tial produe- ' tivity; best suited to needle -leaved trees. Nearly level , some- whatpoorly drained soils that have a sandy sub- soil; on uplands and stream ter- races; moderate potential produe- tivT ! best suited to needle - leave trees. Slash pine Loblolly pine _ Longleaf pine Slash pine _ _ _ Loblolly pine _ Longleaf pine 70 00 70 None recom- mended. None recom- mended. Slash pine, longleaf pine. Slash pine, loblolly pine. Slight Slight early level, very Slash pine ° _ _ _ 70 Swamp Slash pine', Slight poorly drained Loblolly pine' _ 70' tupelo, loblolly soils that have Pond pine' _ _ _ _ 00 sweetgum'. pimne', bald-' sandy underlying cypress, layers; on floodcypress, plains-and stream white terraces; subject cedar. to very frequent flnedine�: moder- _ ' Site eSass is the numerical designation of the relative po- tential productivity of the species shown in the table: It is based on site index, which is the average of the total heights, measured in feet, o£ the dominant and co -dominant trees in an even - aged stand at age 30 for cottonwood, at age 35 for sycamore, and at age 50 for all other species or types. Site index was rounded to the nearest 10 -foot interval to determine site class. Use ®g S®m f®>e Wiidlife2 Wildlife is related to soils through an indirect re - lir ,reship with plants. Wildlife species are associated given types of plant communities which, in turn, By JOHN P. EDWdxDS, biologist, Soil Conservation Service. Moderate _ Mpd- crate. Moderate _ I Mod - crate. Severe' ___� Severe'. For some trees, especially broad-leaved species, site class is based on the comparative site class of other.speeies on the same soil. ' Potential productivity can be attained only where soils have adequate surface drainage. - ' Tree planting is feasible only on areas where surface drain- ageis adequate. Moderate on soils where drainage is adequate, are directly related to particular kinds of soils. Proper manipulation of soil, water, and plants to produce suitable habitat is the most effective way w maintain and improve wildlife population. It is through the three-way relationship of wildlife to plants to soils that interpretations for wildlife are prepared. W SOIL SURVEY The soils of Lenoir County produce a wide variety of plants that provide food, cover, and protection for many species of wildlife. Such upland game species as squirrel, rabbits, quail, mourning doves, foxes, and songbirds are abundant throughout the county. Popu- lations of such furbearers as raccoon, mink, muskrat, and opposum are also abundant. Several species of such waterfowl as mallards, black ducks, and wood ducks are abundant along the Neuse River and Con- tentea Creek and their tributaries. In table 4 the soils in the county have'been rated for seven elements of wildlife habitat. Summary ratings have been made for the three kinds of wildlife for which one might expect to manage..It should be emphasized that the ratings were made using criteria applicable to the individual element. Following is a brief explanation of each element: Grain and seed crops are domestic grains or other seed -producing annuals planted to produce wildlife food. Examples of these are corn, sorghum, wheat, oats barley, millet buckwheat, soybeans, cowpeas, and sun- flowers. Domestic grasses and legumes are domestic peren- nial grasses and herbaceous legumes that are planted for both food and 'cover. Examples are fescue, love - grass, switchgrass, clover, trefoil, and crownvetch. Wild herbaceous plants are native or naturally es- tablished herbaceous grasses and forbs (including weeds) that provide food and cover. Examples are goldenrod, beggarweed, partridge pea, pokeweed, and fescue, . i Hardwood trees are nonconiferous trees and associ- ated woody understory plants that provide food and cover for wildlife species. Examples are oaks, hickory, autumn -olive, dogwoods, and poplar. Coniferous plants are cone -bearing trees and shrubs that furnish wildlife cover or supply food in the form of seed or fruitlike cones. Examples are pine and cedar.. Wetland plants are annual and perennial wild her-' baceous plants of moist to wet sites, exclusive of sub- merged or floating aquatics, that produce food and cover principally for wetland forms of wildlife. Ex-' amples are smartweed, wild millet, rushes, sedges, reeds, wildrice, cutgrass, and cattail. Shallow -water areas rate the suitability of the soil for the creation of shallow -water areas. Surface waters generally have an average depth'of less than 5 feet, They may be naturally wet areas or areas created by dams or levees or by water -control devices in marshes or streams. Examples of such areas are muskrat marshes, beaver ponds, waterfowl feeding areas, and wildlife' ponds. The last habitat element deviates somewhat from the. direct relationship of soils to plants to wildlife. t It is listed, however, because of its primary importance to li to many species of wildlife. area The summary ratings, for the different kinds of wild- life one might expect to find or manage for on a given orate soil are defined as follows: Open -land wildlife.—Birds and mammals that are vege generally associated with open areas or the edges of, ti `,hese areas. These species are found in cultivated areas, favor pastures, lawns, and idle areas overgrown with grasses, be herbs, shrubs, and vines. Mourning doves, quail, red foxes, cottontail rabbits, and many species of songbirds are typical examples of wildlife one might expect to find in this group. Woodland wildlife.—Birds and mammals of wooded areas containing hardwoods or coniferous trees and shrubs, or both. Examples are squirrels, woodpeckers, and gray foxes. Wetland wildlife.—Birds and mammals that are found mainly in such wetland communities as swamps, marshes, or ponds. Examples are.. muskrat, raccoon, redwing blackbird, and various species of ducks. The soils are rated for the three kinds of wildlife using four levels of suitability. This suitability is ex- pressed by an adjective rating that can be defined as follows : Good.—Habitats are easihy improved, maintained, or created. Few or no soil limitations in habitat management exist, and satisfactory results can be expected. Pair.—Habitats can be improved, maintained, or created, but moderate soil limitations affect habitat management or development. A moderate intensity of management and fairly frequent attention may be required to assure satisfactory results. Poor.—Habitats can be improved, maintained, or created, but the limitations are severe. Habitat management may be difficult and expensive and require intensive effort: Results are of question- able value. Very poor.—Under the prevailing soil conditions, it is, impractical to attempt to improve, maintain, or create habitats:' Unsatisfactory results are probable. Such properties as solum thickness, flood hazard, drainage, available water capacity, and slope are con- sidered in malting ratings. When rating soil suitability for wildlife, a two-step procedure is followed. First, the soils are rated for their suitability for producing the seven habitat ole- ments. Then, combinations' of habitat elements are selected and weighed for. their contribution to produc- ing a given kind of wildlife habitat. It should be noted that the ratings given in table 4 are to be used as guidelines and do not provide specific " site analysis. Further. onsite information and analysis will be required when developing individual manage- men plans. Knowledge of soils is necessary in planning, develop= mg, and maintaining areas used for recreation. In able 5 the soils of Lenoir County are rated according mitations that affect their suitability for camp l,. playgrounds, picnic areas, and paths and trails. In table 5 the soils are rated as having slight, mod- , or severe limitations for the specified a uses. For all of these ratings, it is assumed that good cover of tation can be established and maintained. A limita- on of slight means that soil. properties are generally able and limitations are so minor that they'can overcome easily. A moderate limitation can be over- LENOIR COUNTY, NORTH CAROLINA 37 TABLE 4.—Suitability of soils for elements of wildlife habitat and kinds of wildlife Elements of wildlife habitat Kinds of wildlife Soil series Grain Domestic Wild Hard- Conifer- Wetland Open- Wood- Wetland and and grasses herbace- wood one plants Shallow- land land wildlife map symbols' seed and ,ons. trees plants water wildlife wildlife crops leg noes plants areas Bibb: BB ________________ Very Poor ___ Poor ___ Poor ___ Poor ___ Good ___ Good ___ Poor ___ Poor ___ Good. . poor. Blanton: en ________ _____ Poor Fair ___ Good ___ Good ___ Good ___ Poor ___ Very Fair ___ Good ___ Very poor. poor. Chewacla: Ch --- -------- Very Poor ___ Poor ___ Gond ___ Good____ Fair ___ Fair ___ Poor ___ Fair ___ Fair. poor. Colville: Co Poor ___ Fair ___ Fair ___ Fair ___ Fair ___ Good Fair ___ Fair ___ Fail ___ Fair, Craven: Cr, C- ___________ Good ___ Good ___ Good ___ Good ___ Good ___ Poor _.._ Very Good ___ Good ___ Very poor. poor. Goldsboro: Go-,.___ ---- Good ___ Good ___ -Good ___ Good ___ Good ___ Poor ___ P'oor ___ Good ___ Good ___ Poor. Grifton: Or ______________ Poor ___ Fail ___ Fair Fair ---Fair ___ Good ___ Fair ___ Fair ___ Fair ___ Fair. Johns: Jo _____________ Fair ___ Good ___ Good ___ Good ___ Good ___ Poor ___ Very Good ___ Good ___ Very Poor, poor. Johnston: JS _____________ Very Poor ___ Poor ___ Poor ___ Poor ___ Good ___ Good ___ Poor ___ Poor _ Good. poor. Kalmia: Ka, I<b _-------- Fair __- Good ___ Good ___ Good ___ Good -__ Poor ___ Very Good ___ Good ___ Very poor. poor. Kenansville: Ke Fair ___ Good ___ Good ___ Good ___ Good ___ Poor ___ Very' Good ___ Good ___ Very poor. poor. Kinston: Kn _____________ Very Poor ___ Poor Poor ___ Poor ___ Good ___ Fair ___ Poor ___ Poor ___ Fair. poor. Lakeland: La _____________ Very Poor ___ Poor ___ Very Very Very Very Poor ___ Very Very poor* poor, poor, poor. poor. �oor. poor. Leaf: Le _____ ____________ Poor ___ Fair _-- Fair ___ Fair ___ Fair ___ Good ___ Good ___ Pair ___ Fair ___ Good. Lenoir: Ln ____________-- Fair ___ Good ___ Good ___ Good ___ Good ___ Fair ___ Fair ___ Good ___ Good ___ Fair. Leon: Lo Poor ___ Poor ___ Fair ___ Poor Poor _ Poor ___ Very - Poor ___ Poor ___ Very Poor, poor. Lumbee: In _____________ Poor ___ Fair ___ Fair ___ Fair Fair ___ Good ___ Fair ___ Fair ___ Fair ___ Fair. ?" chburg: Ly Poore_-_ Fair ___ Fair ___ Good ___ Good ___ Fair ___ Fair ___ Fair ___ Good ___ Fair. gett: Me _____________ Poor ___ Fair ___ Fair ___ Fail ___ Fair ___ Good___ Pau ___ Fair ___ Fair ___ Fair, lv arville: MU _____________ Very Poor ___ Poor ___ Poor ___ Poor --- Good___ Fair ___ Poor ___ Poor ___ Fair. poor. Norfolk: Na, Nb __________________ Good ___ Good ___ Good ___ Good ___ Good ___ Poor ___ Very Good ___ Good ___ Very poor. poor. No _____________________ Fair ___ Good ___ Good ___ Good --- Good ___ Very Very Good ___ Good ___ Very Poore poor. poor. Pactolus: Pa Good ___ Good ___ Good ___ Good ___ Good ___ Poor ___ Very Good ___ Good ___ Very poor. poor. Pamlico: Pc ____________ Very Poor ___ Poor ___ Poor ___ Poor ___ Good ___ Good ___ Poor ___ Poor ___ Good. poor. Pantego: Pe _______ Very Poor ___ Poor ___ Poor ___ Poor ___ Good ___ Fair ___ Pool-.. Poor -___ Fair. poor. Pocalla: Po Poor Poor ___ Fair ___ Fair ___ Fair. ___ Very Very Poor ___ Fair ___ Very poor. poor. -poor. Portsmouth: Pr ------------ Very Poor ___ Poor ___ Poor ___. Poor ___ Good ___ Fair Poor _ Poor ___ Fair. poor. Rains: Ra _____________ Poor ___ Fair ___ Fair ___ Fair ___ Fair ___ Good ___ Fair ___ Fail Fair ___ Fair. - Stallings: St Fair ___ Good ___ Good ___ Good ___ Good ___ Fair ___ Poor ___ Good __= Good___ Poor.. _ Torhunta: To Very 'Poor ___ Poor ___ Poor ___ Poor ___ Good ___ Good ___ Poor ___ Poor ___ Good. poor. Umbrie Oehraquatfs: Us __ Poor ___ Fair _-- Pair ___ Fair___ Pair ___ Good ___ Fair___ Fair ___ Pair ___ Fair. Wagram: Wb Good ___ Good ___ Good ___ Good ___ Gobd ___ Poor ___ Very Good ___ Good ___ Very poor. - Poore Wagram: We, Wd ----Fail ___ Good ___ Good ___ Good ___ Good'___ Very Very Good ___ Good ___ Very Tool" poor poor. Wickham: Wk ____________ Good___ Good___ Good___ Good___ Good___ Poor___ Very Good___ Good__- Very poor. poor. Weeding Wn ________-- Poor ___ Fair Fair ___ Fair ___ Fair ___ Good___ Poor ___ Fair ___ Fair ___ Fau•. ' All soil's are rated for natural conditions. ' come or modified by planning, by design, or by special door living. Little preparation of the site is required, maintenance. A severe limitation means that costly soil other than shaping and leveli ng for tent and parking - rp`imation, special design, intense maintenance, or a areas. Camp areas are subject to heavy foot traffic c Anation of these is required. and limited vehicular traffic. The best soils have gentle `Camp areas are used intensively for tents and small slopes, good drainage, and a surface free of rocks and canal) trailers and the accompanying activities of out- coarse fragments. The surface is firm after rains but m SOIL SURVEY TABLE 5"—Degree of soil limitations and major features affecting use of soils for recreational development Soil series and Camp areas Pienie areas Playgrounds Paths and trails map symbols Bibb: BB -------- I, Severe: flooding; wet- ness. Blanton: Bn Chewacla: Gh ___ Coxville: Go Craven: Cr, Cv Gcidsboro: Go ___. Griller: Johnston: JS l_ genansville: Ke ___ IIinston: Kn Lakeland: La ______ Leaf: Le _______ Lenoir: Ln ____ Lumbee: Lu Lynchburg: LY -----) Meggett: Norville: Mu Norfolk:' Na, Nb, Nc. ISevere: sand surface layer. __ Severe: flooding; wet- ness. -- Severe: wetness; sur- face ponding where undrained. Moderate: slowpermea bility. - Severe: wetness; sur- face ponding where undrained. Moderate: wetness ---- Severe: flooding; wet- ness. Slight ----------------- Moderate: sandy sur- face layer; subject to blowing. Severe: flooding; wet- ness, ISevere: sand surface layer; subject to blowing. Severe: wetness; su•- faee ponding where undrained, Severe: wetness Severe: wetness; sand surface layer. Severe: wetness.; sur- face ponding where undrained. Severe: wetness Severe: wetness; sur- face ponding where undrained. >evero: wetness; sur- face ponding where undrained. light if slopes are 0 to 8 percent. Coderate if slopes are 8 to 10 percent, Severe: flooding: wet- ness. Severe: sand surface layer. Severe: flooding; wet ness. Severe: wetness; sur- face ponding where undrained. Slight ---------------- Slight ------------- Severe: wetness; sur- face ponding where undrained, Moderate: wetness ____ Severe: flooding; wet- ness. Slight ---------------- Moderate: sandy sur- ' face layer; subject to blowing. - Severe: flooding; wet- ness. Severe: sand surface layer; subject to blowing. Severe: wetness; sur- face ponding where undrained. Severe: wetness Severe: wetness; sand surface layer. Severe: wetness; mr- face ponding where undrained. Moderate: wetness Severe: wetness; sur- e face ponding where undrained. Severe: wetness; sur- face ponding where undrained. Slight if slopes are 0 to 8 percent. Moderate if dopes are 8 to 10 percent. Severe: flooding; wet- ness. Severe: sand surface layer. Severe: flooding; wet- ness. Severe: wetness; sur- face ponding where un- drained. Moderate if slopes are 0 to 6 percent; permea- bility. Severe if slopes are 6 to 8 percent. Slight----------`------ Severe: wetness; sur- face ponding where un- drained. ' Moderate: wetness _____ Severe: flooding; wet- ness. Slight if slopes are 0 to 2 percent. Moderate if slopes are 2 to 6 percent. Moderate: sandy sur- face layer; subject to blowing. Severe: flooding; wet- ness. Severe: sand surface layer; subject to blow- ing. Severe: wetness; sur- face ponding where un- drained. Severe: wetness Severe: wetness; sand surface Iayer. Severe: wetness; sur- face ponding where un- drained. � Severe: wetness ______ Severe: wetness; sur- face ponding where un- drained. Severe: wetness; sur- face pending Where un - [rained: Slight if slopes are 0 to 2 percent. Moderate if slopes are 2 ko 6 percent. Severe if slopes are 6 to 10 percent. Severe: ' flooding; wet- ness. Severe: loose sand sur- face layer. Moderate: flooding; wetness. Severe: wetness; sur- face ponding where un- drained. Slight. Slight. Severe: wetness; sur- face ponding where un- drained. Moderate: wetness. Severe: flooding; wet- ness. Slight. Moderate: sandy sur- face layer. Severe: flooding; wet- ness. Severe: loose sand sur- face layer. Severe: wetness; sur- face ponding where un- drained. . Moderate: wetness. Severe: sand surface layer. Severe: wetness; sur- face ponding where un - mate: wetness. Severe: wetness; sur- face ponding where un- drained. Severe: wetness; sur- face ponding were un- drained. Slight. LLNOIR COUNTY, NORTH CAROLINA 39 T'BLE 5.—Degree of soil limitations and major features affecting use of soils for recreational development —Continued Soil series and Camp areas Picnic areas Playgrounds Paths and trails map symbols ` _ Pactolus: Pa _______ Moderate: wetness, Moderate: we Moderate: wetness; Moderate: sandy sur-. sandy surface layer, sandy surface layer. sandg "surface layer. face layer. Pamlico: Pc _______ Severe: wetness _______ Severe: we _______ Severe: wetness. _______ Severe: wetness, r Pantego: Pe _______ Severe: wetness; sur- Severe: wetness; sur- Severe: wetness• sur- Severe: wetness; sur- face ponding where face ponding where un- face ponding where un- face ponding where un - undrained. drained, drain@d. drained. Pocalla: Po ________ Moderate: sandy sur- Moderate: sandy sur Moderate: sandy sur- Moderate: sandy sur- face layer; subject face layer; subject to face layer; subject to face layer, to blowing* blowing. blowing. Portsmouth: Pr __ _ Severe: wetness; sur-. Severe: wetness; sur- Severe: wetness; sur- Severe: wetness; sur- ' face ponding where ' face ponding where un- face ponding where un= face ponding where un - undrained, drained, drained. drained. Rains: Re _________ Severe: wetness; sur- .Severe: wetness; sur- Severe: wetness; sur- Severe: wetness; sur- face ponding where face ponding where un- face ponding where nn- face ponding where un - undrained. d, ained. drained. drained. Stallings: St _______ •Severe: wetness Moderate: wetness .____ Severe: wetness _______ Moderate: wetness. Torhunta: To ______ Severe: wetness; sur- Severe: wetness- sur- Severe: wetness; sui- Severe: wetness; sur- ` " face ponding where face ponding where un- face ponding where un- face ponding where on. undrained, drained. drained.- drained. Uambrie Ochraqualfs: Severe: wetness; sur- Severe: wetness; sur- Severe: wetness; sur- Severe: wetness; sur- Uo. face ponding where face ponding where un- face ponding where un- face ponding where un - undrained. drained. drained. -'drained. ^am: Wb, We, -Moderate: sandy sur- Moderate: sandy sur- Moderate if slopes are 6 Moderate: sandy sur- vJd, face layer; subject face layer; subject to to 6 percent; sandy face layer. to blowings blowing. surface layer; subject to blowing. Severe if slopes are more than 6 percent. Wielrham: Wk_____ Slight__________________ Slight__________________ Slight if slopes are 0 to Slight. .. 2 percent. - Moderate if slopes are 2 to 6 percent. ' Woodington: Wn ___ Severe: wetness; sur Severe: wetness sur Severe: wetness; sur- Severe: wetness; sur- face ponding where face ponding where un- face ponding where un- face ponding where undrained. drained. drained. & undrained, not dusty when dry, and is Exec from flooding during periods of heavy use. Picnic areas are attractive natural or landscaped tracts used mainly for preparing meals and eating out- doors. These areas are subject to heavy foot traffic. Most of the vehicular traffic, however, is confined to access roads. The best soils are firm when wet but not dusty when dry; are free of flooding during the season of use; and do not have slopes or stoniness that greatly increase -cost of leveling sites or of building access roads. Playgrounds are areas used intensively for baseball, football, badminton, and similar organized games. Soils suitable for this use need to be able to withstand jn- teP'-4ve foot traffic. The best soils have a nearly level s1. ce free of coarse fragments and rock outcrops, gdoa drainage, and freedom from flooding during periods of heavy use. Their surface is firm after rains but not dusty when dry. If grading and leveling are required, depth to rock is important. Paths and trails are used for local and cross-country travel by foot or horseback. Design and layout should require little or no cutting and filling. The best'soils are at least moderately well drained, are firm when wet but not dusty when dry, are flooded not more -than once during the season of use, have slopes of less than 15 percent, and have few or no rocks or stones on the surface. �aagan¢eriag Uses of the S®aLs ' This section is useful to those who need information about soils used'as structural material or as foundation BaLr H. Jo1aEs, civil engineer, Soil Conservation Service, as- sisted in writing this section. SOIL SURVEY upon which structures are built. Among.those who can benefit from this section are planning commissions, town and city managers, land developers, engineers, contractors, and farmers. Among properties -o£ soils highly important in engineering axe permeability, strength, compaction characteristics, soil drainage condition, shrink -swell po- tential, grain size, plasticity, and soil reaction. Also important are depth to the water table, depth to bed- rock, and soil slope. These properties, in various degrees and combinations, affect construction and maintenance of roads, airports, pipelines, foundations for small buildings, irrigation systems, ponds and small dams, and systems for disposal of sewage and refuse. Information in this section of the soil survey can be helpful to those who - 1. 2. 3. 4. 5. 6. 7. Select potential residential, industrial, com- mercial, and recreational areas. Evaluate alternate routes for roads, highways, pipelines, and underground cables. Seek sources of gravel, sand, or clay. Plan farm drainage systems, irrigation sys- tems, ponds, terraces, and other structures for controlling water and conserving soil. Correlate performance of structures already built with properties of the kinds of soil on which they are built, for the purpose of pre- dicting performance of structures on the same or similar kinds of soil in other locations. Predict the trafficability of soils for cross- country movement of vehicles and construction equipment. Develop preliminary estimates pertinent to construction in a particular area. f the information in this section is presented Sin engi- al veering are given in table 6. These estimates are made for typical 'soil profiles, by layers sufficiently different to have different significance for soil engineering. The estimates are based on field observations made in the r: .mcourse of mapping, on test data for these and similar soils, and on experience with the same kinds of soil in other counties. Following are explanations of some of the columns in table 6. Flood hazard is described in terms of the frequency of occurrence and the duration of flooding. Frequency and duration classes are defined in the Glossary. Depth to seasonal high water table is the distance aom.the surface of the soil to the highest level that ground water reaches in the soil in most years. Soil texture. is described in table 6 in the standard terms used by the Department of Agriculture. These terms take into account relative percentages of sand, silt and clay in soil material that is -less than 2 milli- meYers in diameter. "Loam," for example, is soil ma- terial that contains 7 to 27 percent clay; 28 to 50 per- cent silt, and less than 52 percent sand. If the soil contains gravel or other particles coarser than sand, an appropriate modifier is added; for example, "gravelly loamy sand." "Sand," "silt," `clay," and some of the other terms used in USDA textural classification are defined in the Glossary of this soil survey. Liquid limit and plasticity index indicate the effect of water on the strength and consistence of soil ma - everal estimated soil properties significant and others, and the AASHTO system adopted by the American Association of State Highway and Trans- portation Officials (1). In the Unified system (2) soils are classified accord- ing to particle -size distribution, plasticity, liquid limit, qnd organic matter.. Soils are grouped in 15 classes: eight classes of coarse-grained soils, identified as GW, GP, GM; GC, SW, SP, SM, and ,SC; six classes of fine- grained soils, identified as ML, CL, OL, MH, CH, and OH; and one class of highly organic soils, identified as Pt. Soils on the borderline between two classes are designated by symbols for both classes; for example, HL CL. The AASHTO system is used to classify soils accord- ing to those properties that affect use in highway con- struction and maintenance. In this system, a soil is placed in one of seven basic groups ranging from A-1 through A-7 on the basis of grain -size distribution, liquid limit, and plasticity index. In group A-1 are gravelly soils of high bearing strength, or the best soils for subgrade (foundation). At the other extreme, in group A-7, are clay soils that have low strength when wet and that are the poorest soils for subgrade. Where I data are available to justify a further break- down, the A-1, A-2, and A-7 groups are divided as follows: A -1-a, A -1-b, A-2-4, A-2-5, A-2-6, A-2-7, A-7-5, and A-7-6. As additional refinement, the engi- neering value of a soil material can be indicated by a group index number. Group indexes range from 0 for the best material to 20 or more for the poorest. The AASHTO classification is given in table 6 for all soils mapped in the survey area. l properties significant to engineering Most o in tables 6, 7, and 8, which show; respectively, sever estimated soil properties significant to engineering, interpretations for various engineering uses, and re- sults of engineering laboratory tests on soil samples This information, along with the soil map and other parts of this publication, can be used to make inter pretations in addition to those given in table 7. It also can be used to make other useful maps. This information, however, does not eliminate the need for further investigations at sites selected for engineering works, especially works that involve heavy loads or that require excavations to depths greater than these shown in the tables, generally depths greater than 6 feet. Also, inspection of sites, especially the small ones, is needed because many delineated areas of a given soil mapping. unit may contain small areas of other kinds of soil that have strongly contrasting properties and different suitabilities or limitations for soil engineering. Some of the terms used in this soil survey have special meaning to soil scientists that is not known to all engineers. The Glossary defines many of these terms commonly used in soil science. Engineering soil classification systemsThe e two systems most commonly used in classifying samples of soils for engineering are the Unified system used by the SCS engineers, Department of Defense, LENOIR COUNTY, NORTH CAROLINA 41 t iaL As the moisture content of a clayey soil is suitability of the soils for all listed purposes other _eased from a dry state, the material changes from than for drainage of crops and pasture, irrigation, a semisolid to a plastic state. If the moisture content ponds and reservoirs, embankments,and terraces .and is further increased, the material changes from a diversions. For these particular uses, table 7 lists those plastic to a liquid state. The plastic limit is the moisture soil features not. to be overlooked in planning, installa- ' content at which the soil material changes from the tion, and maintenance. Semisolid to the plastic state, and the liquid limit is Soil limitations are indicated by the ratings slight, the moisture content at which it changes from a plastic moderate, and severe. Slight means that soil properties to a liquid state. The plasticity index is the numerical are generally favorable for the stated use or, in other difference between the liquid limit and. the plastic . words, that limitations are minor and can be easily limit. It indicates the range of moisture content within overcome or modified by special planning and design. which a soil material is plastic. Liquid limit and Moderate means that the soils have one or more proper - plasticity index are estimated in table 6. ties unfavorable for a particular use, or that the prob- Permeability is that quality of a soil that enables it lem can be overcome by proper planning, careful to transmit water or au. It is estimated on the basis ' design, and good management. Severe means that soil of those soil characteristics observed in the field, partic- properties are so unfavorable and so difficult to correct ularly structure and texture: The estimates in table 6 or overcome as to require major soil reclamation, -do not take into account lateral seepage or such special designs, or intensive maintenance. For some transient sail features as plowpans and surface crusts. uses, the rating of severe is divided to obtain ratings Available water capacity is the ability of soils to of severe and very severe. Very severe means that one hold water for use by most plants. It .is commonly or more soil properties are so unfavorable. for a partic- defined as the difference between the amount of water ular'use that overcoming the limitations is most diffi- in the soil at field capacity and the amount at the cult and costly, wilting point of most -crop plants. Soil suitability is rated by the terms good, fair, and Reaction is the degree of acidity or alkalinity of a poor, which have, respectively, meanings approximately sail, expressed in pH values. The pH value and terms Parallel to the terms slight, moderate, and severe. used to describe soil reaction are -explained in the In the following paragraphs are explanations of some Glossary.of the columns in table 7. Shrink -swell potential is the relative change in Topsoil is used for topdressing an area where vegeta. volume to. be expected of soil material with changes in tion is to'be established and maintained. Suitability is -ture content; that is, the extent to which the soil affected mainly by ease of worling and spreading the I ! mks as it dries out or swells when it gets wet, soil material, as in preparing a seedbed; natural fer- Extent of shrinking and swelling is influenced by the tBity of the material, or the response of plants when amount and kind of clay in the soil. Shrinking and fertilizer is applied; and absence of substances toxic to swelling of soils'cause much damage to building founda- Plants. Texture of the soil material also affects suit - tions, roads, and other structures. A high shrink -swell ability. Also considered in the ratings is damage that potential indicates a hazard to maintenance of strue- will result to the area from which topsoil is taken. tures built in, on, or with material having this rating.- Sand and gravel are used in great quantities in many Corrosivity, as used in table 6, pertains to potential kinds of construction. The ratings in table 7 provide soil -induced chemical action that dissolves or weakens guidance about where to look for probable sources. A uncoated steel or concrete. Rate of corrosion of un- soil rated as a good source of sand or gravel generally coated steel is related to soil properties such as drain- has a layer at least 3 feet thick, the top of which is Age, texture, total acidity, and electrical conductivity within a depth of 6 feet. The ratings do not take into of the soil material. Gorrosivity for concrete is- in- account thickness of overburden, location of the water fluenced mainly by the content of sodium or magnesium table, : or other factors that affect mining of the ma - sulfate, but also by soil -texture and acidity. Installa- terials; and they do not indicate quality of the deposit. tions of uncoated steel that intersect soil boundaries or Road fill is soil material used in embankments for soil horizons are most susceptible to corrosion than roads. The suitability ratings reflect the predicted installations entirely in one kind of soil or in one soil performance of soil after it has been placed in an horizon. A corrosivity rating of low means that there is embankment that has been properly compacted and a low probability of soil -induced corrosion damage. A provided with adequate drainage, and they reflect the rating of high means that there is a high probability relative ease of excavating the material at borrow of damage, so that protective measures for steel and areas.' more resistant concrete should be used to avoid or Pond reservoir areas hold water behind a dam or minimize damage. embankment. Soils - suitable for pond reservoir areas have low seepage, which is related to their permeability Engineering interpretations of soils and depth to permeable material. The estimated interpretations in table 7 .are based Pond embankments are raised structures of soil ma - on the engineering properties of soils shown in table 6,, nn test data for soils in this survey area and others n` )y or adjoining, and on the experience of engineers ai.,, soil scientists with the soils of Lenoir County. In table 7, ratings are used to summarize limitation or terial constructed across drainageways in order to impound water. These embankments are generally less than 20 feet high, are constructed of `homogeneous" sail material, and are compacted to medium density. Embankments having core- and shell -type construction 42 ' � Soil series ' and map symbols Bibb: BB _____________ Blanton: Bn"________-- Chewaela• Ch __ _ Coxville: Go.__________. Craven: Gr,"Cv ________ Goldsboro: Go _________ Gri£ton:. Gr ____________ Johns: Jo --__--_---__ Sohnston: JS __________ $almia: Ka,�K6 ________ %enansville: Ke ________ SOIL SIIRVEY None. � - 2.5. None, ' 2.5 . Ponding'. 0 None. 1.5 Very fre- .0 quest; ' long periods. Vose. 6 Vose. E 0-13 13-52 52-80 0-12 12-aD 0-15 15-40. 40-70 0-14 14-34 34-65 0-8 " 5-38' 38-60 0-Y4 14-38 38-65 0-24 24-36 ' 36 -SD TABLE 6. Estimated soil properties ' [The symbol > means greater Classification ' � � _ Liquid Plastid USDA Unified AASHTO limit index texture 0 Sandy loam _�. SM, SM -S( .__ Depth to � SM �. Floud. :. seasonal 100 51- 75 hazard: � high Depth SM or SP= frequency; water £rom SM ��duration table � snr£ace SC Ft Ia Frequent; A-4 or A-6 0=45 brie£. 0 45-70 15-25 � Loamy sand _ _ .' None. � "5 " � 0-55 lDD ML, CL or 55-98 NP A�7 � 98-12 Fregnent; 1.5 0-12 brief. 0.6-2.D p.12-0.15 CL 12-27 Sandy loam, �A-4 or A-6�� 27-65 Ponding'. 0 0-12� _ ML -CL or CL Clay loam- :_ -OL' "" Sandy clay � . SG, .CL, 12-62, ML -CL, . A-2 or A-4 62-75 None. � - 2.5. None, ' 2.5 . Ponding'. 0 None. 1.5 Very fre- .0 quest; ' long periods. Vose. 6 Vose. E 0-13 13-52 52-80 0-12 12-aD 0-15 15-40. 40-70 0-14 14-34 34-65 0-8 " 5-38' 38-60 0-Y4 14-38 38-65 0-24 24-36 ' 36 -SD TABLE 6. Estimated soil properties ' [The symbol > means greater Classification ' � � _ Liquid Plastid USDA Unified AASHTO limit index texture 0 Sandy loam _�. SM, SM -S( .__ Loamy sand, � SM NP sand. 100 51- 75 A-4 Sand________ � 8-10 SM or SP= _ _ NE A-4 or A-0 SM " NP -13 Sandy clay 20-30 SC A-2 or A-4 loam, sandy NP -].0 A-4 or A-6 20� 0 loam. " "A-6" � 30-40 15-25 � Loamy sand _ _ SM ' Y00 Loam _______ lDD ML, CL or _ _ NP A�7 � ML -CL 30„8 Clay loam ___. 42-60 CL or ML - 0.6-2.D p.12-0.15 CL __ Sandy loam, �A-4 or A-6�� SM, SC, or' loamy sand. S1VI�C Loam _ _ _ _ _ ML -CL or CL Clay loam- :_ -OL' "" Sandy clay � . SG, .CL, loam. � ML -CL, . A-2 or A-4 or SM -SC Fine sandy ML loam; loam.: 4-11 Clay, clay CH � ' loam. Sandy clay 'SC or CL loam. Loamy sand __ SM ,Sandy clay. �.SM-SC, CL, loam, sandy CL -ML or loam. SC Sandy loam __ SM Sandy clay SC. loam, sandy A-2. or A-3 loam. NP -3 Loamy sand, SM sandy, 'i-2 loam. NP -10 Sandy loam __ SM Sandy clay � SM -SC, SC �� loam, sandy or CL, loam. CL -ML Sand ________ SM or SP -SM Mucky'loam __ OL Fine sandy SM loam, sandy . loam. Sand ________ SM or SP -SM Loamy sand __ SM Sandy clay SC loam, sandy loam. Sand ________ SP -SM or SM Loamy sand __ SM Sandy loam __ SM, SC or SM -SC Loamy sand, SP -SM or sand. SM A 2 or A-4 <35 NP -7 A-2 .__ NP A 2 or A-3 __ NP 60-70 100 51- 75 A-4 18-30 � 8-10 A-2 _ _ NE A-4 or A-0 <40 " NP -13 A-4 or A-0 20-30 4-11 A-2 or A-4 <30 " NP -].0 A-4 or A-6 20� 0 ;4-12 "A-6" � 30-40 15-25 A-4 or A-6. �20-30 �5-15 Y00 51-76 lDD A-4 .. _ _ NP A�7 � � 51-60 30„8 A-7 � 42-60 20-30 0.6-2.D p.12-0.15 A-2 __ NP �A-4 or A-6�� 16-35 '4-Y7 "A� or A-4- <20 NP -3 A-4 or A-6 20-30 8-17 A-2 or A-4 15-30 � NP -3 ' A-2 or A-4 NP A-4 or A-6 - 19-35 4-11 A-2 or A� NP __ IVP A-2 or A-4 <25 " NP -3 A-2 or A-3 _ _ NP A-2 <i6 NP -3 A-2 or A-4 25-30 7-10 A-2. or A-3 <25 NP -3 i-2 <20 NP -3 'i-2 <30 NP -10 1-2 or A-3 __ NP signiftc¢nt in engineering than; <means less than] Perenn No. 4 (4.7 mm) 95-Y00 loo YOD loo lD0 loo 100 96-100 loo I00 YDO 100 100 Y00 100 loo loD 100 100 100 100 100 100 100 100 loo 100 100, 100 loD lab ;age less than 3 inches pae No. 10 No. 40 (2.0 mm) . (0.42 mn ! water 90-100 60-70 100 51- 75 loo 51-7b s5 -loo so so 95-SDO 51-75 100 85-95 100 90-100 96-Y00 60-70 100 85-100 lDD so -1 Do Y00 80-9,5 SOD 75-95 100 �90-Y00 100 80-90 Y00 51-76 lDD sono 95-100 loo- Y00 laD 95-100 so -loo Y00 100 Y00 100 95-100 9D-100 Y00 100 sD-loo 60-95 so-so 51-75 60-70 60-90 51-79 so -loo i0-75 fY-70 .5-90 .5-90 D-lDo 1-75 D -7o 1-75 LENOIR COUNTY, NORTH CAROLINA ,ing sieve - No: 20( (0.074m 30-40 15-sa 5 -Yb 3s -5o 16-30 60-75 70-80 16-40 60-75 7-0-80 36-55 51-65 70-95 36-55 15-3a 36-55 30-40 36-50 20-40 " 30-40 36-5b 6-Y6 80=90 30-45 5-15 Y5.�0 30-50 5-15 15-30 20-35 5-26 2.0-6.0 .60-2.0 .60-2.0 2.0-6.0 0.6-2.0 6.0-20 0.6 2.0 2.0-6.0 6.0-20 2.0-6.0" 0.6-2.0 6.0-2.0 6.0-20 z.o-s.o 6.0-20 0.12-0.15 0.10-6.15 0.12-0.14 O.YO-0.14 Q.Y2-O.Y5 0.03-0,06 I I 0:20-0.26 Oi10-0.14 002-0.06 0:96-0.10 0:12--0.15 1 7.02-0.05 1.05-0.10 LIO-O.Y4 ' 1.02-205 43 Corrosivity Reaetion� Shrink-• swell Uncoated' ' potential steel Concrete PH 4.5-5.5 4.5-5.5 4.5-5.5 4.5-5.5 4.5-5.5 5.1-6.0 5.1-6.0 5.1-6.D 4.5-6.0 4.5-5.6 4.5-5.5 4.5-6.0 4.5-5.5 4.5-5.5 4.5-5.5 4.5-5.5 6.1-5.5 5.1-6.0 6.1-5.4 Low ____ High _: ____ Moderate Low. Low _____'Low ______ High. Low. Low.. Low _____ High _______ Moderate. Low. Low. Low ----- High _--_-- High. Moderate. Low. Q� � High ------� High. Low. Low _____ Moderate ___ High. Low. Low _ _ _ _ � High _ _ _ _ _ _ _I Moderate. Low. Low. 4.5-5.5' Low _ _ _ _ _ Moderate _ _ _ High. Permeability Available ! water n) i capacity ! o� Pei' in I Per hr faoil 0.6-2.0 � � 0.10-0.14 2.a-s.D , D.os-o.lo I 6.0-20 '0.02-0.05 O.G-2.0 10.10-D.13 6.0-20 0.05-0.10 0.6-2.0 ' 0.15-0.19 0.6-2.0 -.0.17-0.19 0.6-2.0 '0.06-0.14 0.6-2.0 - 'O.lb-0.19 4.5-5.5 Low. o.z-D.s o.14-D.la 0.2-0.6 '0.13-0.16 Low ______ X0.12-0.18 0.6-2.0 Low. 0.06-0.2 . X0.12-0.15 0.06-0.2 0.12-0.15 ' 2.0-6.0 I 0.06-0.08 0.6-2.D p.12-0.15 2.0-6.0 .60-2.0 .60-2.0 2.0-6.0 0.6-2.0 6.0-20 0.6 2.0 2.0-6.0 6.0-20 2.0-6.0" 0.6-2.0 6.0-2.0 6.0-20 z.o-s.o 6.0-20 0.12-0.15 0.10-6.15 0.12-0.14 O.YO-0.14 Q.Y2-O.Y5 0.03-0,06 I I 0:20-0.26 Oi10-0.14 002-0.06 0:96-0.10 0:12--0.15 1 7.02-0.05 1.05-0.10 LIO-O.Y4 ' 1.02-205 43 Corrosivity Reaetion� Shrink-• swell Uncoated' ' potential steel Concrete PH 4.5-5.5 4.5-5.5 4.5-5.5 4.5-5.5 4.5-5.5 5.1-6.0 5.1-6.0 5.1-6.D 4.5-6.0 4.5-5.6 4.5-5.5 4.5-6.0 4.5-5.5 4.5-5.5 4.5-5.5 4.5-5.5 6.1-5.5 5.1-6.0 6.1-5.4 Low ____ High _: ____ Moderate Low. Low _____'Low ______ High. Low. Low.. Low _____ High _______ Moderate. Low. Low. Low ----- High _--_-- High. Moderate. Low. Q� � High ------� High. Low. Low _____ Moderate ___ High. Low. Low _ _ _ _ � High _ _ _ _ _ _ _I Moderate. Low. Low. 4.5-5.5' Low _ _ _ _ _ Moderate _ _ _ High. 4.5-5.5 Low. 4.5-5.5 Low, 4.5-5.5 ---------- High ----- High. 4.5-5:5 Low. 4.5-5.5 Low. 4.5-5.5 Low_____ Moderate__ High. 4.5-5.5 Law. 4.5-5.5 Low. 4.5-6.0 Low__.__ Low ______ High. 4.5-5.5 Low. " 4.5-5.5 Lnw. I 44 SOIL SURVEY LENOIR COUNTY, NORTH CAROLINA i TABLE 6. Estimated soil properties significant in engineering -Continued j Soil series and map symbols Flood hazard: _ frequency; duration Depth to seasonal high Depth water from USDA table surface texture Classifieation Unified =- AASHT0 4 Liquid limit Plastici index Ft Fn Mnston: Ko __________ Frequent; 0 0-6 Loam -------- CL A-6 25-35 16-20 . brief 6-50 Clay loam ___ CL - A-6 15-40 12-18 - periods: 50-65 Clay loam _ _ ML, CL or A-4 or A-6, <40 NP -18 ML -CL A2 Lakeland: La --------- None. 5 0-90 Sand ___..___ SP -SM A-2 __ NP Leaf: Le _____________ Ponding. 0 0-10. Loam ______ CL A-4 or A-6 30-40+ 8-15 10-80 Clay, clay CL or CH A-7 41-55 19-37 loam, Lenoir: Ln ___________ None. 1.6 0-11 Loam _---___ ML, CL or A-4 <36.. NP -10 ML -CL ' 11-75 Clay, clay CL A-6 or A-7 30-49 2020 loam. Leon: Lo_____________ None. 1.5 0-14 Sand ________ SP -SM - A-2 or A-3 <24 NP -3 14-37 Sand, loamy SM or A-2 or A-3 <15 NP -3 sand. SP -SM _ ' 37-72 Sand ----- _ _ SP -SM A-2 or A-3 <16 NP -3 Lumbee: Lu __________ Ponding. 0 0-12 Sandy loam _ SM A-2 or A=4 <20 NP -3 12-38 Sandy clay SC or A--4 or A-6 19-35 4-15 loam, sandy SM -SC loam. 38-65 Sand________ SP -SM or A-2 or A-3 NP SM Lynchburg: Ly________ None. _, 1,5 0-12 Sandyloam_ SM A-4 or A-2 .<25 NP -3 - 12-85 Sandy clay SO or CL, A-4 or A-6 20-40 4-16 loam. ML -CL, SM -SC Meggett: Me _________ Ponding. 0 0-12 Fine sandy SM A-2 or A-4 __ NP ' loam,sandy loam. 12-45 Clay, sandy SC, CL or A-7 45-65 25-40 clay, sandy CH clay loam, 45-85 Sandy clay SC A-4 or A-6 25-44 7-20 loam. Murville: Mu _________ Ponding, 0 0-58 Fine sand ___ SP -SM A-2 or A-3 NP . 58-87 Loamy fine SM A-2 __ _ _ NP sand. Norfolk: Na, Nb, No __ None. 5 0-12 Loamy sand _ . SM A-2 <16 NF -3 12-85 Sandy clay SC, SM -SC, A-4 or A-6 <35 4.-15 loam. CL, CL - ML Pactolus: Pa None. 1-2.5 0-38 Loamy sand _ SM A-2 __ NP 38-75 Sand_______ SM or A-2 orA-a NP SP -SM __ _ Pamlico: Pc __________ Veryfre- 0 0-33 Muck Pt NP quent; __ 33-65 Loamy sand, SM or __ A-2 __ long sand. SP -SM periods, Pantego: Pe __________ Ponding. 0 - 0-14 Loam,sandy ML, SO or A-4 <40 NP -10 loam.. CL -ML - 14-74 Sandy clay' SC or CL A-6 25-35 11-25 loam, Pocalla: Per _____.____ None. 5 0-22 Loamy sand, SM or A-2"orA-3 NP sand. SP -SM __ 22--40 Sandy loam _ SM, SCOT A-2 <80 NP -10 SM -S C I 40-66 Sand A-2 or A-3 NP SP -SM _, 66-80 Sandy loam _ SM, SC or A-2 «0 NP -10 SM -SC Percentage Iess than 3 inches passing sieve- Corrosivity 'y Permeability (Available Reaction Shrink- No. 4 - No. 10 No. 40 No. 200water swell Uncoated ac (4.7 mm) (2.0mm) (0.42 mon) (0.074 mm) ' ca capacity r -potential steel Concrete lln e an 7n Per Ar f Boil PH I 100 100 85-95 60-75 2.0-6.0 0,15-0,20 4.5-5,5 Low ----- High _ _ _ _ _ __ High, 100 100 90-100 70-80 0.6-2.0 0.15-D.26 4.6-5.6 Low. 1.00 90-100 90-100 70-80 0.6-2,0 0412-0.16 4.5-5.5 Low 100 100 51-70 5-12 6.0-20 i 0.02-0.05 4.5-5,0 Low _____ Low _______ Moderate. 100 100 85-95 60-76 0.06-.20 , 0.15-0.20 4.6-5.5 Low ____ Very high High. 100 100 90-100 75-95 0.06-,20 0.15-0.20 4.5-5,5 Moderate, 100 100 85-98 60-85 0.6 2.0 . 0.15-0.20 4.5-5,5 Low _ _ _ _ High _ _ _ _ _ _ _ High. 100 100 90-100 60-95 0.06-,20 - 0.15-0-18 4.5-5,6 Moderate, 100 100 80-100 5-12 6:0-20 0.02-0,05 4.0-5,5 YeTylaw Low _______ High. 100 100 80-100 5-20 2.0-6.0 0.05-0,10 4.0-5,5 Very low. 100 100 80-100 5-12 600-20 0.92-0.05 4.0405 Very low. 100 100 60-70 . 30-40 2.0-6.0 0.10-0.12 4.6-6.0 Low _ _ _ _ High _ _ _ _ _ _ _ High. 100 96-100 65-90 36-50 0,6-2.0 0.12-0.15 4.6-5.5 Low. 100 .90"100 51-70 5-15 6.0-20 0.03-0.06 4.5-5.5 Low, 100 100 60-70 "30-49 2.0-6.0 0.16-0.14 40-6,0 Low ____ High _______ .High. 100 100 80-90 36-55' 0.6-2,0 012-0.15 4,0-5.5 Low, 100 100 60-85 30-49 2.0-6,0 0.10-0.15 6.6-6.5 Low ____ Very high __ Low. 100 96-100 80-95 45-75 0.06-0,2 0.15-0.18 6.1-&4 High, 100 95-100 70-90 36-50 0.06-0,2.,0.15-0.18 6.6-8,4 Moderate. 100 100 65-80 5-12 6,0-20 10.06-0.08 4.0-5,0 Low ____ High _______ High. 100 100 51-76 15-30 2.0-6,0 0.06-0.08 4.04,0 Low. 100 100 51-75 15-30 2.0-6.0 '0.06-0.08 4.5-5.5 Low____ Low _______ High. 100 100 80-90 36-55 0.6-2,0 0.12-0.15 4,5-5,5 Low, 100 100 51-75 15-30 6.0-20- :0.06-0.10 4.54.5 Low ____ Low _______ High, 109 100 51-70 6-15 6,0-20 X0.02=0.05 4,5-5,5 Low. , -- -- -- -- 0.6-2,0 &24-0.26 4.0-5,5 ---- High ---'-- High, 100 100 51-75 10-30 2.0-6,0 0,03-0.08 4.0-5,5 Low. a 100 100 65=100 36-65 2:0-640 15-0,17 4.0-5.5 Low____ High_______ High, 100 96-100 80-100- 36-56 0.6-2,0 p.13-015 4,0-5,5 Low. I 100 100 51-97 5-30 6.0-20 0,05-0.10 4.6-6,0 Low ____ Low _______ High. 100 100 60-97 20-40 0.6-2.0 0.10-0.14 4.5-5.5 Low. 100 100 51-97 5-20 6.0-20 0.05-0.08 4.5-5.5 Low. 100 100 60-97 30-40 0.6-2,0 0.10-0.14 4.5-5.5 Low. L 1 �' 46 SOIL SURVEY " TABLE 6. Estimated soil properties Soil series and ' Flood hazard: Frequency; Depth to seasonal high water Depth from USDA Classification Liquid limit Plasticity index -Unified�•� AASHTO map symbols duration � table surface texture piping and in sandy sub- 61=75 erosion. stratum at a (1.06-0.08 depth of about Low. 45 inches. 100 95-100 51-70 Portsmouth: Pr Ponding 0 0-13 Loam ____ __ ML or A-4 �. 20-40 3-10 ________ 4.0-5.5 Low. Y00 100 ML -CL 60-70 30-40 2.0-6.0 0.08-0.12 4.5-6.0 Low _ _ _ _ _ High _ _ _ _ _ _ " Higb. 13-38 � Sandy clay SC or A-4 or"A-6 19-35 4-15 soils -Continued 100 100 loam, sandy SM -SC 0.62.0 0.10-0.14 4.5-5.5 Low. 100 95-100 60-70 loam: 0.6-2.0 0.11-0.15 4.5-5.5 Low. Excavated ponds Dwellings 38-70 � Sand ________ SP -SM or A-2 orA-3 __ NP filter fields lagoon) and streets industries (trench and SM 3ains: Ra Ponding 0 0-13 Sandy loam __ SM, SC or A-2 or A-4 <20 NP -10 _____________ able flood I flooding; flooding; sea- flooding; sea - permeability. conal high SM -SC damage to poorly conal high conal high water table. water table. 13-63 Sandy clay SC or � A-4 15-30 4-20 moderately moderately loam. SM -SC rapid perrhe- rapid perme- 63-85 Sandy clay SC A-2 or A-6 20-40 11-20 substratum at substratum at loam. a depth of� � � - a depth of Stallings: 5[ ___________ None. 1 0-12 Loamy sand _ SM A-2 __ NP inches: � '� ' ' ' 12-42 Sandy loam _ SM A-2 or A-4 <25 NP -3 42-80 Loamy sand _ SM A-2 _ _ NP To Ponding. 0 0-14 Loam ______ ML A-4 __ NP .'orhunta: __________ 14-36 Sandy loam _ SM A--4 or A-2 _ _ NP 36-65 Loamy sand, SM or A-2 or A� _ _ NP sand. SP -SM Jmbrie Ochraqualfs: Frequent 0 0-14 Loam ______ ML, CL, A-4 <40 NP -YO Uo. Ponding. CL -ML 14-70 � Sandy clay CL or SC "A-6 or A-7 30-4$ 15-30 . loam, sandy clay. �agram: Wb, Wc, Wd __ None. 5 0-30 Loamy sand __ SM A-2 <20 NP -3 30-90 Sandy clay SC, SC -SM A-4 or A-6 21-30 5-12 loam. Tickham: Wk� _________ None. 6 � 0-15 Loamy sand _ SM A-2 __ � NP 15-43 Sandy clay SC, SC -SM, � A-4 <30 NP -10 loam, sandy SM loam. 43-65 Loamy sand _ SM A-2 NP _ _ �oodington: Wn _____ Ponding. 1 0-12 Loamy sand _ SM A-2 NP 12-47 Sandy loam _ SM, SC or A-4 or A-2 <30 NP -10 SM -SC 47-85 Loamy sand _ SM A-2 NP 'Shallow water commonly stands during or £olIowing a rain. Suitability as source of - Soil series and map symbols Topsoil Sand Gravel Road fill Bibb: BB ______ P'oor: poorly -Poor: impxob- Poor: improb-�' Poor: poorly drained, able source. able source. drained. i TABLE 7. Interpretations of [Dashes indicate that information is not Limitations for - Pond 85-95 reservoir Pond areas embanj�ents 4.0-5.5 Low _ _ _ _ _ High _ _ _ _ _ _ High. Severe: mod- Moderate: poor eratety rapid resistance to permeability piping and in sandy sub- 61=75 erosion. stratum at a (1.06-0.08 depth of about Low. 45 inches. 100 ' � LENOIR COUNTY, NORTII CAROLINA 47 svgniftcant in engineering -Continued ,'I Percentage less than 3 inches passing sieve- ' Corrosivity Permeability Available .Reaction Shrink - No. 4 No. 10� � No. 40 No. 20D water � swell Uncoated �. (4.7 mm) (2.0 mm) (0.42 mm) (0.074 mm) �eapaeity potential steel' Concrete 100 100. 85-95 15-30 60 -?5 D.6-2.0 ,0.14-0.18 4.0-5.5 Low _ _ _ _ _ High _ _ _ _ _ _ High. 100 95-100 60-85 36-50 0.62.0 O.Y3-0.15 4.5-5.5 Law. 100 61=75 15-30 6.6-20 (1.06-0.08 4.5-5.5 Low. 100 100 95-100 51-70 5-15 6.D-20 ;0.02-O.DS 4.5-5.5 Low. 100 60-70 30-40 2.0-6.0 0.10-0.16 4.0-5.5 Low. Y00 100 100 60-70 30-40 2.0-6.0 0.08-0.12 4.5-6.0 Low _ _ _ _ _ High _ _ _ _ _ _ " Higb. 95-100 -.51-75 15-3D 6.0-20 0.06-0.10 4.5-5.5 Low. enginee��ing properties of the soils -Continued 100 100 80-90 36-50 0.62.0 0.10-0.14 4.5-5.5 Low. 100 95-100 60-70 30-40 0.6-2.0 0.11-0.15 4.5-5.5 Low. Excavated ponds Dwellings Septic -tank � Sewag¢ Local roads Light Sanitary landfill' �. (aquifer fed) filter fields lagoon) and streets industries (trench and Y00 100 51-75 15-30 6.0-20 0.06-0.10 4.5-5.5 Low -____ Moderate__ High. 100 100 60-70 30-40 2.0-6.0 0.10-0.14 4.5-5.5 Low. 100 100 61=75 15-30 6.6-20 (1.06-0.08 4.5-5.5 Low. 100 � 100 85-95 60-75 2.0-6.0� 0.10-0.15 4.0-5.5 Low _ _ _ _ _ High _ _ _ _ _ _ High. Y00 100 60-70 30-40 2.0-6.0 0.10-0.16 4.0-5.5 Low. Y00 95-100 51-75 5-25 6.0-20 - 0.02-0.05 4.0-5.5 Low. ' 100 100' 51-75 150 6.0-20 0.06-0.08 4.5-6.0 Low_____ Low ______ High. 100 96-109 60-90 3fi-50 2.0-6.0 0.13-0.15 4.5-5.5 High ______� Low. lOQ I .100 I 80 95 � .I 36-60 I 0,6-2.0 10.15-017 100 I 6.1-8.4 36-50 I Moderate.) Low. 100 100' 51-75 150 6.0-20 0.06-0.08 4.5-6.0 Low_____ Low ______ High. 100 96-109 60-90 3fi-50 2.0-6.0 0.13-0.15 4.5-5.5 Low. . 100 100 ,51-75 15-30 2:0-6.0 0.06-0.10 5.1-6.6 Low--___ Low ______ Moderate. 100 160 60-90 36-50 0.6-2.0 0.13-O.lb 5.1-6.5 Low. 90-100 90-100 51-7D 1520 6,0-20 0.05-0.16 5.1-6.5 Low. - lOD 100 61-75 15-30 6.020 6.06-0,10 Low___=_ High______ High. I00 100 60-76 30-40 .4.5-5.5 2,6-6.6 0;10-0.14 � 4.5-5.5 Low. 100 95-100 -.51-75 15-3D 6.0-20 0.06-0.10 4.5-5.5 Low. enginee��ing properties of the soils -Continued available or that the practice is not applicable] .. Degree of limitations and major soil feiatures affecting selected.use- Excavated ponds Dwellings Septic -tank � Sewag¢ Local roads Light Sanitary landfill' �. (aquifer fed) filter fields lagoon) and streets industries (trench and area method) Moderate: Severe: Severe: � Severe: prob- Severe: Severe: Severe: moderate � flooding; sea- flooding; sea- able flood I flooding; flooding; sea- flooding; sea - permeability. conal high conal high damage to poorly conal high conal high water table. water table. embankment; drained. water table. water table; ' moderately moderately rapid perrhe- rapid perme- ability; sandy " ability; sandy substratum at substratum at ' a depth of� � � - a depth of about 45 I about 45 inches. inches: � '� ' ' ' C 4 J J -q 48 SOIL SURVEY TABLE 7. Interpretations of LENOIR COUNTY, NORTH CAROLINA 49 i engineering properties of the soils—Continued Excavated ponds (aquifer fed) Seveie: deep to water table in dry season. Severe: rapid permeability in substratum. Moderate: depth to water table in dry season. Moderate: depth to water table in dry season; slowly perme. able aquifer. Moderate: depth to water table in dry season. Moderate: depth to water table in dry season; marl substra- tum. Moderate: depth to water table in dry season. Degree of limitations and major soil features affecting selected use Dwellings Septic -tank filter fields Slight __________ Slight ________ ISevere: flooding; sea- sonal high water table. Severe: sea- sonal high water table. Severe: clayey subsoil. Moderate: sea- sonal high water table. Severe: sea- sonal high water table. Severe: sea. sonal high water table. Slight -------- __I Severe: flooding; sea- sonal high water table. ievere: depth Slight ------ to water table in dry season, Severe: depth I Slight ------- to water table in dry season. Severe: flooding; sea- sonal high water table. Severe: sea- sonal high water table; moderately slow perme- ability. Severe: sea- sonal high water table; slow perme. ability. Severe: sea- sonal high, water table. Severe: sea- sonal high water table, Severer sea- sonal high water table. Severe: flooding; sea- sonal high water table. Slight ________ Slight Moderate: moderate permeability, Severe: j depth to seasonal high water table.' Severe: depth to seasonal high water table. Severe: .depth to seasonal high water table. ! I Severe: depth to seasonal high water table. Severe: .depth to seasonal high water table. Severe: depth to seasonal hi gh water table; sandy subtratum at a depth! of about 34 inches; •rapid permeability. Severe: flooding; - rapid perme- ability (sea- sonal high water table. t Severe: rapid permeability; sandy stibstra- tum at a depth of about 38 aches. Severe: rapid permeability; sandy sub- stratum at a depth of about 36 inches. Local roads Light and streets industries Slight ________ Slight ------ Severe: flooding, I Severe: poorly drained; clayey tex- ture. I.Severe: clayey tex- ture. Slight _ Severe: poorly drained. Moderate: somewhat poorly drained. Severe: flooding; very poorly drained. Right Slight ----- Severe: flooding; sea. sonal high water table. Severe: sea- sonal high water table; clayey sub- soil. Severe: clayey subsoil. Moderate: sea- sonal high water table. Severe: sea- sonal high water table. Severe: sea- sonal high water table. Severe: flooding; sea- sonal high water table. Slight if 0• to 4 percent slopes., Moderate if 4 to 6 percent slopes. Slight if 0 to 4 percent slopes. Moderate if 4 to 8 percent slopes. Sanitary landfill (trench and area method) Slight. Severe: flooding; sea- sonal high water table. Severe: sea- sonal high water table. Severe: sea- sonal high water table. Severe: sea- sonal high water'table. Severe: sea- sonal high water table; marl substra- tum. Severe: sea- sonal high water table; rapid uerme- ability; sandy substratum at a depth of about 34 inches. Severe: sea- sonal high water table; flooding; rapid .- permeability; sandysub- stratum at a depth of about 38 inches. Severe: sandy substratum at a depth of about 38 inches; rapid permeability. Severe: rapid permeability; sandy sub- stratum ata depth of about 36 inches. Suitability as source of— Limitations for— Soil series Pond and map Topsoil Sand Gravel Road. fill reservoir areas Pond embankments symbols 3lanton: Bn Poor: sand Poor: execs- Poor: improb- Good ___.------ Mmoderate der resistance poor Moderate: ..- surface layer. sive fines. able source. permeability, piping and erosion. lhewacla: Ch -- Good . -------- Unsuited: ex- Unsuited: ex- fines; Fair: some- Moderate: moderate Moderate: good to poor . cessive.fines; high cessive seasonal high what poorly drained. permeability. resistance to seasonal water table; water table; piping and subject to subject to erosion; _me- dium compress flooding; prob- flooding; ibility, able source probable below depth of source below about 4 feet. depth of about 4 feet. loxville; Co ._- Fair:, limited Unsuited: ex- Unsuited: ex- Poor: poorly drained, Slight ____----- Moderate:medium m- _ amount of cessive fines. cessive fines. pressibility; suitable ma- fair slope terial. stability. ;raveni' Cr, Cv Fair: limited Unsuited: ex- Unsuited: " ex- Poor: low Slight _____----- Moderate: edium com- - amount of cessive fines. cessive fines. slaength, pressibility; suitable ma- fair slope terial. stability. foldsboro: Go Poor: loamy Poor: improb- Poor: improba- Good --- _------- Moderate: SlightSlight__________ _ sand surface able source: ble source. permeability-. layer. Gr-____ Poor: Poor:. improb- Poor: improba- Poor: poorly Moderate: Moderate: good to :Tifton: poorly drained. able source. ble source. drained. moderate permeability. poor resist - ance to piping and erosion. Jo Good. Poor: exces- Poor: excessive Fair: some- Severe: rapid Moderate: good to ohns: - .__ _ sive fines; fines; probable what poorly permeability; poor re - to probable source below drained. sandy substra- sistanee source below depth of about time at a depth of 34 piping and erosion; ' depth of about 4 feet, inches. medium 4 feet, .. permeability. Poor: very Poor: improb- Poor: improba. Poor: very Severe: rapid Severe: poor ohnston: JS __ able source. ble source. poorly permeability; resistance to poorly drained. sandy sub- piping. drained. stratum at a _ depth of about 38 inches. :almia: Ka, Poor: loamy 'Poor: excessive Poor: excessive Good ___________ Severe: rapid Moderate: good to poor re - Kb, sand surface fines; proba- fines; proba- ble be- permeability in sandy sub- sistance to layer. ble source below depth source low depth of stratum at a piping and of about 4 about 4 feet. depth of about erosion. feet. 38 inches. :enansville: - Poor: loamy Fair: few fines. Poor: ' excessive fines; Good ___________ Severe: rapid permeability• .Moderate: medium Ke, sand surface proba- ble source be- sandy sub- permeability; layer. y low depth of stratum at a poor resist - about 4 feet, depth of about I ante to piping 36 inches. I and erosion. LENOIR COUNTY, NORTH CAROLINA 49 i engineering properties of the soils—Continued Excavated ponds (aquifer fed) Seveie: deep to water table in dry season. Severe: rapid permeability in substratum. Moderate: depth to water table in dry season. Moderate: depth to water table in dry season; slowly perme. able aquifer. Moderate: depth to water table in dry season. Moderate: depth to water table in dry season; marl substra- tum. Moderate: depth to water table in dry season. Degree of limitations and major soil features affecting selected use Dwellings Septic -tank filter fields Slight __________ Slight ________ ISevere: flooding; sea- sonal high water table. Severe: sea- sonal high water table. Severe: clayey subsoil. Moderate: sea- sonal high water table. Severe: sea- sonal high water table. Severe: sea. sonal high water table. Slight -------- __I Severe: flooding; sea- sonal high water table. ievere: depth Slight ------ to water table in dry season, Severe: depth I Slight ------- to water table in dry season. Severe: flooding; sea- sonal high water table. Severe: sea- sonal high water table; moderately slow perme- ability. Severe: sea- sonal high water table; slow perme. ability. Severe: sea- sonal high, water table. Severe: sea- sonal high water table, Severer sea- sonal high water table. Severe: flooding; sea- sonal high water table. Slight ________ Slight Moderate: moderate permeability, Severe: j depth to seasonal high water table.' Severe: depth to seasonal high water table. Severe: .depth to seasonal high water table. ! I Severe: depth to seasonal high water table. Severe: .depth to seasonal high water table. Severe: depth to seasonal hi gh water table; sandy subtratum at a depth! of about 34 inches; •rapid permeability. Severe: flooding; - rapid perme- ability (sea- sonal high water table. t Severe: rapid permeability; sandy stibstra- tum at a depth of about 38 aches. Severe: rapid permeability; sandy sub- stratum at a depth of about 36 inches. Local roads Light and streets industries Slight ________ Slight ------ Severe: flooding, I Severe: poorly drained; clayey tex- ture. I.Severe: clayey tex- ture. Slight _ Severe: poorly drained. Moderate: somewhat poorly drained. Severe: flooding; very poorly drained. Right Slight ----- Severe: flooding; sea. sonal high water table. Severe: sea- sonal high water table; clayey sub- soil. Severe: clayey subsoil. Moderate: sea- sonal high water table. Severe: sea- sonal high water table. Severe: sea- sonal high water table. Severe: flooding; sea- sonal high water table. Slight if 0• to 4 percent slopes., Moderate if 4 to 6 percent slopes. Slight if 0 to 4 percent slopes. Moderate if 4 to 8 percent slopes. Sanitary landfill (trench and area method) Slight. Severe: flooding; sea- sonal high water table. Severe: sea- sonal high water table. Severe: sea- sonal high water table. Severe: sea- sonal high water'table. Severe: sea- sonal high water table; marl substra- tum. Severe: sea- sonal high water table; rapid uerme- ability; sandy substratum at a depth of about 34 inches. Severe: sea- sonal high water table; flooding; rapid .- permeability; sandysub- stratum at a depth of about 38 inches. Severe: sandy substratum at a depth of about 38 inches; rapid permeability. Severe: rapid permeability; sandy sub- stratum ata depth of about 36 inches. 50 Soil series and map symbols Topsoil Kinston: Kn _ Poor: poorly drained. Lakeland: La _ Poor: sand surface layer. Leaf: Le ---- Poor: poorly drained. - Lenoir: Ln ___ Fair: limited amount of suitable ma- terial. Leon: Lo ----- Poor: sand surface layer. Lumbee: Lu __� Poor: poorly drained. Lynchburg:, Ly Faix: limited amount of material. Meggett: Me' _ Poor: poorly drained. Murville: Mu_ _.f Poor: very poorly drained. SOIL SURVEY Suitability as source o£— Sand Gravel Poor: excessiv fines; seasons high water table; subject to flooding; probable source below depth of abou� 4 feet. Fair: few fines. Unsuited:ex- cessive fines. Unsuited: ex- cessive fines. Fair: few fines. Poor: exees- sive fines; seasonal high water table; subject to flooding; prob- able source be- low depth of about 4 feet. Poor: improb- able source. Unsuited: ex- cessive fines. Fair: exces- sive fines and organic -matter content. Poor: exces- sive flues; sen sonal high water table; subject to flooding; prob able source below depth in about 4 feet. Poor: improb- able source. Unsuited: ex- cessive fines. Unsuited: ex- cessive fines. Poor: improb- able source. TABLE 7. Interpretations of Poor: exces- Limitations for— . Severe: rapid Moderate: Pond drained. permeability; Road fill reservoir Pond water table: sandy sub- areas embankments Poor: poorly Moderate: Moderate: good drained. moderate to poor re- erosion; suit. permeability. sistance to 38 inches. able material piping and water table. erosion; me- below depth dium eom- ' of about 4 pressibility. Good _______--- Severe: rapid Severe: poor permeability. slope sta- Poor: improb- Fair: some- bility; high Moderate: poor - permeability; moderate resistance poor resist- drained. ance to piping piping. Unsuited: ex- and erosion. Poor: poorly Slight -------- Moderate: hig drained. compressi- shrink -swell bility. Fair: some- Slight ------- Moderate: what poorly row material. high com- drained. pressibility. Fair: some. Severe: rapid Severe: poor what poorly permeability; slope sta- drained. sandy sub- bility; high stratum at a permeability; depth of about poor resist - 37 inches. ance to piping and erosion. Poor: exces- Poor: poorly . Severe: rapid Moderate: sive flues; drained. permeability; seasonal high good to poor seasonal high water table: sandy sub- resistance to , water table; seasonal high tratum at a piping and subject to surface depth of about erosion; suit. flooding; prob- Severe: sea- 38 inches. able material able source water table. at a depth of below depth about 38 , of about 4 inches. feet. Poor: improb- Fair: some- Moderate: Moderate: poor able source. what poorly moderate resistance to drained. permeability. piping. Unsuited: ex- Poor: poorly Slight __________ Moderate: cessive fines. drained; high thickness of shrink -swell suitable bor- potential. row material. Poor: improb- Poor: very able source. poorly drained; high content of organic mat- ter. Severe: mod- Severe: poor erately rapid slope sta- permeability. - bility; high permeability; poor resist- ance to piping and erosion, I Sl LENOIR COUNTY, NORTH CAROLINA engineering properties of the soils—Continued riegree of limitations and ajor soil features affecting selected use— Excavated ponds Dwellings Septic -tank Sewage -Local roads Light landfills' (aquifer fed) filter fields lagoons and streets industries (trench and area method) Moderate: Severe: Severe: Severe:. Severe: Severe: Severe: depth to flooding; sea- flooding; sea- $oodvrg; .flooding; flooding; sea- flooding; sea- water table in sonal high sinal high seasonal high poorly sonal high sinal high dry season, water table. water tableo water' table, drained. water table, watetable. ISevere: depth to water tabloid dry season. ISevere: very slow perm ab lity of aqu fer: Severe: slow permeability of aquifer. Moderate: - depth to water table in dry season. Moderate: depth to i water table in dry season. Zoderate: depth to water table in dry season. Moderate: depth to water table in dry season. ght--------- S. Slight --------- Slight ----- Severe: mod- Severe: slow crate to high permeability; shrink -swell seasonal high Potential; water table: clayey subsoil; seasonal high water table; surface ponding. Severe: sea- Severe: sea - sinal high sonal high water table. water table 'Severe: sea- sonal high water table. Severe; sea- sonal high water table. .evere: sea- sonal high water table, evere: sea- sonal high water table; high shrink - swell pot os- tial. :Vere: sea- sonal high water table. slow perme- ability, Severe: sea- sonal high water table. Severe: sea- sonal high water table. Severe: sea- sonal high water table. Severe: sea- sonal high water table; slow perme- ability. Severe: sea- sonal high water table. __I Severe: rapid permeability, I Severe: sea- sonal high water table. I Severe: sea- sonal high water table, Severe: sea- sonal high water table; rapid perme- ability, sandy substratum at a depth of 37 inches. Severe: sea- sonal high water table; rapid pezme- ability, sandy substratum at a depth of about 38 inches. Severe: sea- sonal high water table. )evere: sea sonal high water table. Severe: sea- sonal high water table; moderately rapid pernne- ability, Slight I Severe: Poorly drained. I Severe: Unified group is CL. Moderate: somewhat poorly drained. Severe: poorly drained. Moderate: somewhat poorly drained. ;evere, poorly drained; high shrink - swell poten- tial. evere: very poorly drained. Slight if 0 to I Percent slope Moderate if 4 ti 8 percent slopes. Severe: sea - sinal h gh water table; clayey; mod- erate shrink - swell poten- tial. I Severe: sea- sonal high water table. Severe: sea- sonal high water table. Severe: sea- sonal high water table. Severe: sea- sonal high water table. Severe: high shrink -swell potential seasonal kigh water table, levere: sea- sonal high water table. Severe: rapid permeability. Severe: sea- sonal high water table. I Severe: sea- sonal high water table. Severe: sea- sonal high water table; rapid perme- ability; sandy substratum at a depth of about 37 inches. Severe: sea- sonal high water table; rapid perme- ability;sandy substratum at a depth of about 38 inches. Severe: sea - sinal h gh water table. Severe: sea- sonal high water table; marl substra- tum, evere: sea sonal high water table; moderately rapid perme- ability. 51 52 i Soil :ser., map symE. Topsoil Norfolk: Na, Nb, No. Pactolus: Pa Pamlico: Pc _ Pantego: Pe Pocalla: Po --- Portsmouth: Pr, Rains: Ra _____I Poor: loamy sand surface .layer. _) Poor: loamy sand surface layer. 1 Poor: very poorly drained. Poor: very poorly drained. Poor: loamy sand surface layer. Poor: very poorly drained. Poor: poorly drained. SOIL SURVEY Suitability as source of— Sand Gravel Poor: improb- able source. Fair: some fines. Poor: improba- ble source. Poor: improba- ble source. Poor: exces- sive fines. Poor: exces- sive fines; Probable source below depth of about 4 feet. Poor: improba-.I ble source. Stallings: St ___ Poor: loamy Poor: impxoba- sand surface ble source. - layer. Poor: improb- able source. Poor: improb- able source. Poor:improb- able source. Poor: improb- able source. Poor: improb- able source. Poor: improb- able source. Poor: improb- able source. Poor: improb- able source. TABLE 7. Interpretations of Limitations for— Pond Pd-I reservoir Pond areas embankments Moderate: Slight moderate permeability. . Fair: some- what poorly drained. Poor: very poorly drained; or- ganie surface layer. Poor: very poorly drained. Good Poor: very poorly drained. Poor: poorly drained. _Fair: some- what poorly drained. Severe: rapid permeability. Severe: mod- erately rapid permeability; sandy sub- stratum at a depth of 33 inches. Moderate: moderate permeability. Severe: rapid permeability; sandy sub- stratum at a depth of about 40 inches. Severe: rapid permeability; sandy sub- stratum at a depth of about 38 inches. Moderate: Moderate: poor resist- ance to piping and erosion; Poor slope stability; me- dium to high permeability, Severe: poor slope sta- bility; high compressi- bility. Slight_____ Moderate: in dium perrui ability; poor resistance to piping and erosion. Moderate: good to poor resistance to piping and erosion; suit- able material at a depth of about 38 inches. Slight _________ moderate Legree of limitations and major soil £e permeability.: Dwellings Septie-tank Sewage Severe: rapid 7 to Moderate: lagibns permeability; Slight if 0 to 8 poor resist - Moderate if i sandy sub- percent ante to piping 7 percent stratum at a slopes. and erosion; slo es mb depth of about Severe if more medium per - ability. 42 inches, meability; Percent slopes. Moderate: fair slope Severe: sea - somewhat sonal high stability, Poorly drained. 1! LENOIR COUNTY, NORTH CAROLINA engineering properties of the soils—Continued I Moderate: depth to water table it dry season. Slight Slight__________ Severe: deep to water table in dry season, Slight--- doderate., depth to water table in dry season, loderate: depth to water table in dry season. Moderate if Legree of limitations and major soil £e Excavated ponds Dwellings Septie-tank Sewage (aquifer fed) 7 to filter fields lagibns Severe: deep Slight if 0 to 8 Slight if 0 to 8 Moderate if i to water table in percent percent slopes. 7 percent dry season. slopes. Moderate if slo es mb I Moderate: depth to water table it dry season. Slight Slight__________ Severe: deep to water table in dry season, Slight--- doderate., depth to water table in dry season, loderate: depth to water table in dry season. Moderate if more than 8 Crate gerii m more than 8 percent slopes. ability;, percent Severe if 7 to slopes, Slight. percent slog Severe: sea- Severe: sea- Severe: sea- sonal high sonal high sonal high water table. water table, water table slopes. " rapid perme Severe if more ability. Severe: sea- sonal high water table, surface ponding and flooding. Severe: sea- sonal h gh water table. Slight Severe: _ sea- sonal high water table. severe: sea- sonal high water table. evere: sea- sonal high water table.,, Severe; sea- sonal high water table; flooding, leveret aea- sonal high water table. light --------- Severe: sea. serial high water table. Severe: sea_ sone] high water table. Severe: sea- sonal high water table. Severe: sea- sonal high water table; flooding; high in content of organic mat- ter; mod- erately rapid permeability; sandy sub- stratum at a depth of 33 inches,I Severe: 'sea- sonal high water table. Severe: rapid Permeability; sandysub- stratum at a depth of 40 inches. Severe: sea- sonal high water table; rapid perme- ability; sandy subtratum at a depth of about 38 inches. :were• sea- sonal high water table, vere: sea- I sonal high water table; moderately lapid perme- Lbility; sandy ubstratom t a depth of bout 42 aches. res affecting selected use— Local roads Light Sanitary landfill' and.streets industries (trench and area method) Slight if 0 to 8 Slight if 0 to 4 Slight. percent percent slopes. slopes. Moderate if 4 to Moderate if 8 8 percent to 10 percent slopes. " slopes. Severe if more than 8 to 10 Percent slopes. Moderate: Severe: sea- Severe: sea - somewhat sonal high sonal high Poorly drained. water table. water table; rapid perme- ability. ISevere: very poorly drained; flooding. Severe: very poorly drained. Slight ________ Severe: very I poorly drained. severe:" poorly drained . federate: somewhat poorly drained. Severe: sea- serial high water table. Severe: sea- serial high water table. Slight if 0 to 4 Percent slopes. Moderate if 4 to 8 percent slopes. Severe: sea- sonal high water table. Severe: sea- sonal high water table. evere: sea- sonal high water table. Severe: sea - serial high water table; flooding; mod- erately rapid permeability; sandy substra- tum at a depth of 33 inches, Severe: sea- sonal high water table, Severe: rapid permeability; sandy substra- tum at a depth of 40 inches, Severe: sea- sonal high water table; rapid perme- ability; sandy substratum at a depth -of about 38 inches, Severe: sea- sonal high water table. Severe: sea- sonal high water table; moderately rapid perme- ability, sandy substratum at a depth of 42 inches. 53 SOIL SURVEY TABLE 7.—Interpretations of ' Onsite studies of the underlying ssrasa, waver L Suitability as source of— Limitations for— Soil series .percent 55 engineering properties of the soils Pond hold sewage within a depth of 2 to 5 feet long enough .and map symbols — Topsoil Sand Gravel Road fill reservoir Pond embanlanents embankment is compacted to medium density and the Severe: depth Slight --------- Slight ---------- to water table areas Sanitary Torhunta: To __ Poor: very Poor: improba- Poor: improb- Poor: very poorly Severe: rapid permeability; - Moderate: poor resist- (aquifer fed) poorly ble source, able source. drained, sandy sub- once to piping - dxained. stratum at a and erosion; Slight __________ ' Severe: sea- Severe: sea- Severe: very depth of about medium per - . sonal high sonal high sonal high poorly 36 inches, meability; water table. water table. water table; drained. water table. fair slope rapid perme- " stability. Umbric Poor: very Unsuited: ex- Poor: improb- Poor: very Moderate: moderate Slight:. very poorly Ochraqualfs: poorly cessive fines. able source, poorly drained, permeability. drained. UO, drained, a depth of a depth of Wagram: Wb, Poor: loamy Fair: probable Poor: improb- Good ----------- Severe: mod- erately rapid Moderate: poor resist - We, Wd, sand surface source. able source, permeability. anee to layer, PIPMs• Wickham: Wk_ Poor: loamy Poor: exces- Poor: exces- Good___________ Severe:rapid Mooaresist- poor sand surface sive fines; sive fines; probable permeability; sandy sub- anee to piping. L layer. probable source below source below stratum at a depth of about depth of about depth of about , 4 feet. 4 feet. 43 inches. Woodington: Poor:*poorly Poor: excessive Poor: improb- Poor: poorly drained. Severe: rapid permeability; Moderate: resist- p oor Wn. drained. fines, able source. sandy sub- • ante to piping ' stratum at a and erosion; depth of 47 medium per - inches. meability; fair slope stability, a.,, , ==u are not rated in this table: Embankment foundation, reservoir area, and slope are assumed to be suitable for pond construction. Soil properties that affect the em- bankment and the availability of borrow material are considered. The best soils have good slope stability, low permeability, slight compressibility under load, and good resistance to piping and are thick enough for easy excavation,' An aquifer -fed excavated -pond (fig. 12) is a body of water created by excavating a pit or dugout into a ground -water aquifer. Excluded are ponds fed by run- off and also embankment -type ponds where the depth of water impounded against the embankment exceeds 3 feet. The assumption is made that the .pond is properly designed, located, and constructed and that the water is of good quality. Properties affecting quifer-fed ponds are the existence of a permanent water table, permeability of the aquifer, and properties that interfere with excavation, such as marl. Dwellings (without basements), as rated in table 7, are not more than three stories high and are supported by foundation footings placed in undisturbed soil. The features that affect the rating of a soil for dwellings are those that relate to capacity to support load and resist settlement under load, and those that relate to ease of excavation. Soil properties that affect capacity to support load are wetness, susceptibility to flooding, density, plasticity, texture, and shrink -swell potential, Those that affect excavation are wetness, slope, and depth to marl. Septic tank filter fields are subsurface systems of tile or perforated pipe that distribute effluent from a septic tank into natural soil. The soil material,ffrom a depth of 1� inches to 6 feet is evaluated. The soil properties considered are those that, affect both absorption of efduent and construction and operation of the system. Properties that affect absorption are permeability, depth to water table, and susceptibility to flooding. Slope is a soil property that affects difficulty of layout and: construction and also the risk of soil erosion; Slight: maz•1 Severe: sea - substratum somal high interferes water table. with excava- tion in places. Severe: sea- Severe: "sea- sonal high I sonal high water table. water table. Severe: depth Slight if 0 to S LENOIR COUNTY, 14ORTII CAROLINA .percent 55 engineering properties of the soils Moderate if 8 to hold sewage within a depth of 2 to 5 feet long enough Moderate if 8 to 15 percent Slight if �0 to 8 Degree of limitations and major soil features affecting selected use— slopes. embankment is compacted to medium density and the Severe: depth Slight --------- Slight ---------- to water table ' Sanitary Excavated ponds Dwellings Septic -tank Sevtage. Local roads Light landfill' (aquifer fed) filter fields lagoons and streets industries (trench and - traffic all year. They have a subgrade of underlying area method) Slight __________ Severe: sea- Severe: sea- Severe: sea- Severe: very Severe: sea- Severe: sea- . sonal high sonal high sonal high poorly sonal high sonal high water table. water table. water table; drained. water table. water table; rapid perme- rapid perme- ability; sandy ability; sandy substratum at substratum at a depth of a depth of about 36 ahout 36 inches. inches. Slight: maz•1 Severe: sea - substratum somal high interferes water table. with excava- tion in places. Severe: sea- Severe: "sea- sonal high I sonal high water table. water table. Severe: depth Slight if 0 to S Slight i£ 0 to 8 to water table .percent percent slopes. in dry season. slopes. Moderate if 8 to hold sewage within a depth of 2 to 5 feet long enough Moderate if 8 to 15 percent Slight if �0 to 8 15 percent slopes. pacted soil material. The assumption is made that the slopes. embankment is compacted to medium density and the Severe: depth Slight --------- Slight ---------- to water table ' Those that affect the pond floor are permeability, in dry. season. organic matter, slope, and.depth to marl (if marl is t Moderate: Severe: sea- Severe: sea - depth to water somal high somal high table in dry water table. water table. season* need to be made for landfills deeper than 5 to 6 Severe• mod- erately rapid permeability. Severe: (rapid permeability; sandy ¢ub- stratum at a depth of 43 inches: Severe: Y sear somal O a - lateral seepage, and downslope flow of. effluent. Soils Severe: sea - that are underlain by sandy layers have the potential somal high risk of contaminating nearby water supplies. drained, Sewage lagoons are shallow ponds constructed to water table, hold sewage within a depth of 2 to 5 feet long enough for bacteria to decompose the solids. A lagoon' has a Slight if �0 to 8 nearly level floor, and sides, or embankments, of com- Severe: mod - pacted soil material. The assumption is made that the percent slopes. embankment is compacted to medium density and the slopes. P(is protected from flooding. Properties that -affect permeability. the pond floor and the embankment' are considered. 8 percent Those that affect the pond floor are permeability, ` organic matter, slope, and.depth to marl (if marl is t present). The soil properties that affect the embark- Severe if more ment are the engineering properties of the embank- slopes. ment material as interpreted from the Unified soil classification. . slopes. Local roads and streets, as rated in table 7, have an all-weather surface expected to carry automobile traffic all year. They have a subgrade of underlying Severe: very Severe: sea- Severe: sea - poorly somal high sonal high drained, water table, water table, Slight if �0 to 8 Slight if 0 to 4 Severe: mod - percent slopes. erately rapid slopes. Moderate if 4 to permeability. Moderate if 8 percent MOT than slopes: - S percent Severe if more slopes. than 8 percent . slopes. Slight ____ Severe: Poo drained. Severe: sea- sonal high N Slight________ ater table. Severe: rapid permeability; sandy substra- tum ata depth of about 43 inches. Severe: sea- - .sonalhigh water table; rapid perme- ability; sandy substratum at a depth"of 47 inches. soil material; a base consisting of gravel,'crushed rock, or soil material stabi&zed with. Ione or cement; and a fiexible or rigid surface, commonly asphalt or concrete. These roads are graded to shed water and have ordinary provisions for drainage. They are built mainly from soil at hand, and most cuts and fills are less. than 6 feet deep. Soil properties that most affect design and construc- tion of roads and streets are load -supporting capacity and stability of the subgrade , and the workabffity and quentity of out and fill material available.. The AASH and. Unified classifications of the soil lila- . aerial, and also the shrink -swell potential, indicate load - supporting capacity. Wetness and. flooding affect. sta- . bility of the material. Slope, depth to marl, and wetness affect ease of excavation and amount of cut and fill needed to reach an even grade. Ratings for light industry (fig. 13) are for the undisturbed soils that are used to support building foundations. Emphasis is on foundations, ease of exca- 56 SOIL SURVEY - LENOIR COUNTY, NORTH CAROLINA 57 TABLE g,-- Engineering test data _ [Tests performed by North Carolina State Highway Commission, Department of Materials and Tests, Raleigh, N.C.] Moisture -density' Mechanical analysis' Classification Soil name Parent Report No. Percentage g and location material S70NC54– Depth Maximum Optimum I g passing sieve— Percentage smaller than- dry density moisture Lquid Plasticity No. 10 No, 40 No. 200 0.05 0.02 0.005 0.002 - limit index AASHTO' Unified mm) (0,074 n,mmm m ) m mm mm 1% Pot Pct Coastal Plain sediment. 5-1 0-8 107 16 100 97 69 61 50- 27 j 16. 25 5 A-4(7) CL -ML Coxville loam: 5-3 12-27 109 17 100 98 81 75 66 4438 37 20 A-6 (12) CL 2 miles southeast of LaGrange, 04 mile 6-6 62-75 122 11 100 91 40 37 29 22 1 19 22 7 A-4(1) SC stof and State intersection ad f1 27, 0.3 Highway 70e " southeast of State Road 1327, and 20 feet southwest of farm road. (Modal) - Old Coastal Plain alluvium. 13-1 0=8 112 11 100 90 20 18 12 6 4 16 NP ° A-2-4(0) SM Salmia loamy sand: 13-4 16-28 115 14 100 88 36 34 30 26 28 29 9 A-4(•0) SC 4 miles northeast of Kinston, 0.2 mile 13-7 43-65 101 16 100 99 11 9 7 6 4 24 NP A-2-4(0) SM -SP east of inon of N,C1 5 and State Ro dtersec1810,tiand 2 fe t south of State Road 1810. (Modal) Coastal Plain sediment and old 14-2 8-22 109 12 100 97 13 11 9 6 4 17 NP A-2-4(0) SM Pocalla loamy sand: .14-4 26-40 118 11 100 97 24 22 21 17 15 17 NP A-2-4(0) SM 7 miles south of LaGrange, 0.6 mile east alluvium. 14-6 40-66 101 15 ( 100 97 17 7 4 3 2 22 NP A-2-4(0) SM of intersection of N.C. Highway 55 and State Road 1002, and 20 feet north of N.C. Highway 55. (Modal)' Coastal Plain sediment. 19-1 0-6 102 16 100 .90 11 9 6 3" ' 2 24 NP A-2-4(0) SM -SP Leon sand: 19-3 14-19 117 10 100 89 17 16 14 9 6 15 NP A-2-4(0) SM 5 miles east "of Pink Hill, 0.6 mite east of intersection of State Road 1105 and State Road 1118, and 25 feet south of State Road 1106. (Modal) 107 15 ± 100 98 81 70 53 26 15 25 3 A-4(8) y fine sandy loam: Coastal Plain sediment. YS -1 0-8 18-4 21-48 ( ) ML 8 miles east of Sinton and 50 feet south- 104 20 i 100 99 89 81 69 51 41 49 27 A-7-6 (17) CL Lenoir ver west of intersection of State Road south - 18 -6 62-75 109 16 . 100 98 66 60 50 39 34 41 23 A-7-6 (lY) CL 1806 and State Road 1807. (Modal) - Coastal Plain Sediment - 2 -1 0-9 88 26 -E 100 95 52 47 40 23 15 38 9 A-4(3) ML Pantego loam: 2-4 19-50 112 15 99.5 95 51 47 43 34 2S 27 15 A-6 5) CL 9.5 miles south of Kinston, 1.2 miles 2-6 64-74 113 14 99 94 46 41 33 31 28 30 13 A-6(3) SC southwest of intersection of State Road _ 1922 and State Road 1925, and 25 feet northeast of State Road 1922. (Modal) _ calculations of grain -size fractions. The mechanical analyses used in this table are not suitable for use in naming textural 'Based on AASHTO Designation T 99, Method A and i (1). classes for soil. ° Mechanical analyses according to the AASHTO Designation T 88 (Y p cedts o f this procedure frequently may differ somewhat from results that world have been obtained by the soil survey procedure of the Soil Conservation Service (SCS). Based on A STM Stand, Designation 6 1(2), (1). xe cal - in the ed on the O pro ed r ,t e finermateri riding that ao rsernthan 2 moillimete ster oinadia et r. In thnd the variouse SCS s it survey procedure, ractions a- ' NP emeans onplae. D 2457-69 (.E). the fine material h; analyzed by the pipette method and. the material coarser than 2 milometers in diameter is excluded from vation" far underground utilities, and corrosion po- ular traffic. Some soil properties that affect suitability tential of Uncoated steel pipe. The undisturbed soil is for landfill are ease of excavation, hazard of polluting rated'for spread footing foundations for buildings less ground water, and trafliicabilitwithste deet soils trhave e, than three stories high or foundation' loads not in moderately slow permeability, excess of that weight. Properties affecting -load-sup- and are friable and easy to excavate. Unless otherwise porting capacity and settlement under lanndd shr nketswell about6 feet a d, therefore, limitation nly nratings ofy to a s light th of flooding, texture, es of eit i density, behavior. Properties affecting excavation are wetness, or moderate .may not be valid if trenches are to be flooding; slope, and 'depth to marl. Properties affecting much deeper than that. For some soils," reliable pre - corrosion of buried uncoated steel pipe are wetness, diectardless of that -,be ions can everye to a site should be investigateth of 10 or 15 feet; d xture, total acidity, and electrical resistivity.. g Sanitary landfill is a method of disposing of refuse before it is selected, in. dug trenches. The waste is spread in thin layers, Soil test data compacted, and covered with soil throughout the dis- posal period. Landfill areas are subject to heavy vehic- Table 8 contains engineering test data for some of the major soil series in Lenoir County. These tests were mum dry density. As a rule, maximum strength of made to help evaluate the soils for engineering pur- earthwork is obtained if the soil is compacted to the poses. The. engineering classifications given are based maximum dry density. on data obtained by mechanical analyses and by tests Tests to determine liquid limit and plasticity index to determine liquid limits and plastic limits. The me- measure the effect of water on the strength and con- ehaoical analyses .were made by combined sieve and sistence of the soil material, as has been explained for hydrometer methods. table 6. Moisture -density (or compaction) data are important in earthwork. If a soil material is compacted at suc- cessively higher moisture content, assuming that the Formation and* Classification compactive effort remains constant, the density of the of the So' ts compacted material increases until the optimum moil. Lure content is reached. After that, density decreases Any one soil has a unique combination of a great , w th increase in moisture content. The highest dry many soil characteristics. An individual soil, as one density obtained in the compactive test is termed maxi- individual body on the landscape, varies in the size of 60 SOIL SURVEY _- along the large drainageways. As fallen leaves, twil roots, and whole plants decay, plant nutrients and c ganic acids are released to percolate down through t soil horizons. Roots take up some of the nutrients. C game 'acids act to dissolve the more slowly'solut mineral components and hasten the rate of removal soluble inorganic materials from the surface horizor The effect of these organic acids on soil formation conditioned by climate. Climate modifies the rate chemical reaction and the rate of leaching and, to large degree, determines the kinds of plants and an mals living in and on the individual kinds of soil. Organic matter decays more rapidly in the surfai horizons of such well -drained soils as the Norfol. Wagram, and Kenansville soils because the periods saturation are shorter than they are for the poorl drained soils. There is very little accumulation of a ganic matter in the surface horizons of the wel drained soils, and their surface horizons remain light colored. Decay of organic matter is retarded in the surface horizons of the poorly drained soils, such Portsmouth, Torhunta, Murville, and Johnston because the periods of saturation last from one da to several weeks each year. The excess moisture re- tards tards the oxidation, allowing wet soils to accumulate high content of organic matter in the surface horizon, This causes the surface to be darker colored than th surface of well -drained soils. Also, the organic matter probably is the energy source for micro-organisms involved in oxygen con- sumption in saturated A horizons. The wet soils have 'anger periods of saturation, and the biological activity can reduce the oxygen levels of the ground water s anaerobic conditions can exist for several days o weeks. The reducing conditions along with the saturation are postulated to be responsible for gray colors in th subsoil of the poorly drained soils. Time The sequence of horizons in the soil profiles requires a long time to develop. Some of the differences among the kinds of soils reflect differences in their age. Older soils generally have better defined horizons than young soils. In Lenoir County the older Norfolk, Wagram, and Goldsboro soils on the smoother, nearly level up- land divides have well-developed horizons. These nearly level soils have formed in Coastal Plain surfaces that are essentially unchanged for as much as 10 million years or since Upper Mocene time. - - By contrast the more recent -soils, -such-as Bibb,- Kinston, Johnston, and Chewacla, formed in alluvium that has not been in place long enough to develop well- defined horizons. Relief The relief in Lenoir County is largely the result of dissection by the Neuse River and. its tributary streams. Landscape dissection, acting through its in-' fluence on water table depths and geologic removal of soil material by slope retreat, affects the formation of oils in Lenoir County. The deepest water tables are near the short, sharply xounded side slopes: Deep water tables are associated with thick A2 horizons, fine -textured B horizons, bright colors in the B horizons, and a decrease in and eventual disappearance of bodies low in content of clay. The Wagram and Norfolk soils reflect those characteristics that are associated with well drained conditions. The shallow water tables are associated with thin A2 horizons, low -contrast mottling, and presence of bodies low in content of clay. The soils in the interstream areas, such as Lynchburg, Rains, and Pantego, reflect those characteristics that are associated with high water tables: The removal of soil material by geological erosion has caused the solum of soils that formed on side slopes to remain thin. .iiiu� ml il�r �n�il� 1_ Soils are classified so that we can more easily re- member their significant characteristics. Classification enables us to assemble knowledge about the soils, to as see their relationship to one another and to the whole soils, environment, and to develop principles that help us to y understand their behavior and their response to ma- nipulation. First through classification, and then a through use of soil maps, we can apply our knowledge of soils to specific fields and other tracts of land. e The narrow categories of classification, such as those used in detailed soil surveys, allow us to organize and apply knowledge about soils in managing farms, fields, and woodlands; in developing rural areas; in engineer- ing work; and in many other ways. Soils are placed in broad classes to facilitate study and comparison in o large areas such as countries and continents. r The system of soil classification currently used was adopted by the National Cooperative Soil Survey in 1965 W5 (y)> (8)• e The Soil Taxonomy has six categories. Beginning with the broadest, these categories are order, suborder, great group, subgroup, family, and series. In this sys- tem the criteria used as a basis for classification are soil properties that are observable and measurable. The properties are chosen, however, so that the soils of similar genesis, or mode of origin, are grouped. In table 9 the soil series of Lenoir County are classified according to the Soil Taxonomy. Classes of the Soil , Taxonomy are briefly defined in the following para- graphs. ORDER. Ten soil orders are recognized. The proper- ties used to differentiate among soil orders. are those that tend to give broad climatic groupings of soils. The tLree-exceptions to this are the-theIneeptisols; - and Histosols, which occur in many different climates. Each order is named with a word of three or four syllables ending in sol. sSDBORDER. Each order is subdivided into suborders that are based mainly on those soil characteristics that seem to produce classes with the greatest genetic sim- ilarity. The suborders narrow the broad climatic range ' permitted in the orders. The soil properties used to separate suborders are mainly those that reflect either the presence or absence of waterlogging, or soil differ- ences resulting from the climate or vegetation. The names of suborders have two syllables. The last sylla- ble indicates the, order. LENOIR COUNTY, NORTH CAROLINA 61 TABLE 9. Soils classified according to current system Series Family Subgroup I Order Bibb _______>______________ Taxadjunets to the Lenoir series because the combined thickness of A and Bl horizons ranges from Coarse -loamy, siliceous, acid, thermic ___ Typic Pluvaquents Entisols. Blanton ------ __------- _----- Loamy, siliceous, thermie _______________ ___________________ Grossarenie Paleudults Ultisols. ' Chewacla ___________ Fine -loamy, mixed, thermic _ __ Fluvaquentic Dystrochrepts __________ Inceptisols. Coxville ________________ Clayey, knolinitic, thermic _'___________ Typic Paleaquults Ultisols. Craven ______________________ Clayey, mixed, thermic ------- -------- _ ____ Aquic Hapludults Ultisols. Goldsboro ---- _------ _------- Fine -loamy, siliceous, thermic _________ ____________________ Paleudults Ultisols. Grafton ___________�. _________ Fine -loamy, siliceous, thermic __________ .Aquic _____________________ Typic Ochraqualfs Alfisols. Johns _______________________ Fine -loamy over sandy or sandy -skeletal, ____________________ Aquic Hapludults Ultisols. - siliceous, thermic. ---------------- Johnston _ __________ Coarse -loamy„ siliceous, acid, thermic ____ Cumulie Humaquepts _____ Inceptisols. Aalmia ___----------- __ "Fine -loamy over sandy or sandy -skeletal, Typic Hapludults Ultisols. siliceous, thermic. _____________________ Kenansville __________________ Loamy, siliceous, thermic ______________ Arenic Hapludults ____________________ Ultisols. Kinston _____________________ Fine -loamy, siliceous, acid, thermic ______ Typic Fluvaquents _________ Entisols. Lakeland ___________ Thermic, coated ______________________ Typic Quartzipsamments _____________ Entisols. Leaf _______________ Clayey, mixed, thermic _________________ Typic Albaquults Ultisols. Lenoir_ _____________________ Clayey, mixed, thermic _________________ __________ Aeric Paleaquults Ultisols. Leon ________________________ Sandy, siliceous, thermic _______________ ___________________ Aeric Haplaquods ___________________ Spodosols. Lumbee ________________ Fine -loamy over sandy or sandy -skeletal, Typic Ochraquults Ultisols. " siliceous, thermic. ___________________ Lynchburg ___________________ Fine -loamy, siliceous, thermic _______:_ Aeric Paleaquults ___________________ UItisols. Meggett ___________________ Fine, mixed, thermic _________________ Typic Albaqualfs ____________________ Alfisols. Murville __________________ Sandy, siliceous, thermic ______________ Typic Haplaquods ________:__________ Spodosols. Norfolk ____________________ Fine -loamy, siliceous, thermic _________ Typic Paleudults Ultisols. Pactolus ____________________ Thermic, coated ______________________ ____________________ Aquic Quartzipsamments Entisols. Pamlico _____________________ Sandy or sandy-skeletal,.siliebous, dysic, __ Terrie Medisaprists ' thermic. _____________ " -Histosols. Pautego _____________________ Fine -loamy, siliceous, thermic __________ Umbrae Paleaquults Ultisols. Pocalla ______________________ Sandy, siliceous, thermic ______________" _____________ Axenic Paleudults Ultisols. Portsmouth __________________ Fine -loamy, siliceous, thermie _________ __________ Typic Umbraquults ______ U'ltisols. Rains ___ Fine -loamy, siliceous, thermic _________ Typic Paleaquults Ultisols. Stallings ____________________ -Coarse-loamy, siliceous, thermic ----- Z_ __________________ Aerie Paleaquults Ultsols. Torhunta ____________________ Coarse -loamy, siliceous, acid, thermic ____ ___________________ Typic Humaquepts __________________ Inceptisols. T�liram _____________________ Loamy, siliceous, thermic ______________ Arenic Paleudults Ultisols. ham ____________________ Fine'loamy, mixed; thermic _____________ _______________ Typic Hapludults Ultisols. V. .dington __________________ Coarse -loamy, siliceous, thermic ________ ______ Typic Paleacfuults ____________________ Ultisols. 10 to 74 inches in about 70 percent of the unit, and the character of change in texture between the A and the BZt horizon is on the limit to an abrupt textural change. GRPviT GROUP. Soil suborders are -separated into group mainly on the basis of properties important to great groups on the basis of uniformity in the kinds the growth of plants or on the behavior of soils when and sequence of major soil horizons and features. The used for engineering. Among the properties considered horizons used to make separations are those in which are texture, mineralogy, reaction, soil temperature, clay, iron, or humus have accumulated; those that have permeability, .thickness of horizons, and consistence. pans that interfere with growth of roots, movement A family name consists of a series of adjectives pre - of water, or both; and thick, dark -colored surface hori- ceding the subgroup name. The adjectives are the class zons. The features used are the self -mulching proper- names for texture, mineralogy, and so on, that are used ties of clay,. soil temperature, major differences in as family differentiae as shown in table 9. chemical. composition (mainly calcium, magnesium, sodium, and potassium), dark -red and dark -brown colors associated with basic rocks, and _the like. The _ _G.eeyal Nature f -the. ® tp� namesss of great groups have Three or four syllables and are made by adding a prefix to the name of the sub- This section gives general facts about Lenoir Coun- order. ty. It briefly discusses physiography, relief and'drain- SUHGROUP.. Great groups are subdivided into sub- age; water supply; climate; settlement and develop - groups, one representing the central (typic) segment meat; transportation; and industry. of the graup and others called intergrades that have properties of the group and also one or more proper= Physiography, g$�lfef, and Drainage ties bf another great group, suborder, or. order. Sub- groups may also be made in those instances where soil Lenoir County is in the Coastal Plain physiographic properties intergrade outside of the range of any other province. The soils are underlain by unconsolidated great group, -suborder, or order. The names of sub- sand, silt, and clay except for small intermittent areas gi s are derived by placing one or more adjectives on the southeast side of the county. *These small areas be ,,re the name of the great group. are underlain by friable to weakly cemented, greenish - FAMILY. Soil families are separated within a sub- gray marl that has a high content of sand, Most of bVater m , mttucture ENVIRONMENTAL OUALITY PAT MCCRORY DONALD R. VAN DER VAART KEM H. COLSON City o J 30 Box 4 Subject: Engineering Report Funding Approval City of Kinston Briery Run Sewer Rehabilitation Phase IV Project No.: CS370527-11 The IDivision of Water Infrastnrcture (Division) has completed its review of the subject engineering report. Eased upon this review, the Division has determined that the referenced project is eligible for funding as follows: Elignble Rehabilitation of the Briery Run Sewer Olutfali Line between Airport Road and Wallace Family Road to include lining of approximately 4,295 linear feet of 30 - inch gravity sewer via CIDP; and 49 manholes; installation of permanent access to the sewer easement, stabilization of stream banks and erosion control. Based upon detailed review o£ the bid documents, it may be determined that portions of the project are not eligible for funding and the total loan amount maybe reduced. in accordance with G.S. 120-157.1 through 157.9, enacted on June 24, 2011, local government units with projects that require debt to be issued greater than $1,000,000 must submit a letter to Committee Chairs, Committee Assistant, and the Fiscal Research Division of the General Assembly at least 45 days prior to presentation before the Local Government Commission. You are responsible for submitting this letter and providing a copy to the Division, Projects funded through the CWSddF program must comply with the federal Brooks Act €or the selection of architectural, surveying, and engineering services. CWS}21F projects cannot be exempted from qualification based selection of these services under N.C.G.S.143-64.32. The Professional Engineering Services Procurement form on our website will need to be submitted as documentation of compliance for any services to be reimbursed. Any services provided that were not selected in compliance with federal requirements will be ineligible for reimbursement. t dr. Sears, City Manager November 1, 2016 Page 2 of 2 Please note that the milestones bellow must be met to ma am assurance of funding under the State Revolving ]Fund. Bid and Design Package Submittal: May 1, 2017 Bid and Design Package Approval: September 1, 2017 Advertise Project, Receive Bids, Submit Bid Information, and January 2, 2018 Receive Authority to Award: Execute Construction Contract(s): February 1, 2018 if you have any questions concerning this matter, please contact Anita E. Reed, PE by email at anita.reed@ncdenr.gov or at (919) 707-9174. Sin�cerel�y,_ }) Seth Robertson, PE, Chief State Revolving Fund Section Attaclunent cc: John Jarrell, PE, City Engineer, Kinston NC Mark Hubbard, PE via email Anita E. Reed, PE Susan Kubacki via email James Baltzer, PE SRF (BRJfaW RAL) �' 'Nothing Compares: �_ Slate ofNonh Cazolina � Envrtoomenml Quality�Wacer ln6aswcnae 1633 Mail Service Ceater, Raleigh, Nonh Carolina 27699 � Location 512 N. 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Ia 2 m i ESTNUT S7 12 CHr- ep u —' - _ E CORDON ST 'sU5 W R H -e�F y .~ V E CASWELL Sr W CASWELL ST o 05 W RD -� E KING ST ZJ CEDAR LN - - �'• ,. 11 - Z� 70 55 258 Bus Maplewood d ry�,���,. , I i - t _ ."5 Ii ti's f-. ° sY• \ ESHI \_ 1-25 X25' -- - CI N LINCOLN ST LL25 850000 ._ _...> ._ Ls- - __ bPyp° .z`' - -_ -�- _ - W 25 04 N FEET UNIVERSITY ST y - _. �. 55 70 Bus M '•zs. __. _ - 15 70 - - _ - Tj 15 �l 5 'I`- 25 35015' I,= _ _ U i 35°15' 35°t6' '62 363 26412 420 000 FEET -- '66 267 366 '69 '70 '71 '72"`-E 77°37'30" 35' 32'30" 77030' Produced by the United States Geological Survey * SCALE 1:24 000 ROAD CLASSIFICATION North American Datum of 1983 (NAD83) Expressway Local Connector Worid Geodetic System of 1984 (WGS84). Projection and 1 0.5 0 KILOMETERS 1 2 NORrR 1 000-meter grid: Universal Transverse Mercator, Zone 18S q• 4y• ROLINA A. Secondary Hwy LOcaI Road 10 000-foot ticks: North Carolina Coordinate System of 1983 172 MILS 1000 500 0 METERS 1000 2000 Ram 4WD q• 0 1 p This map is not a legal document Boundaries may be MR! generalized for this map scale. Private lands within government MILES .Interstate Route US Route O State Route reservations may not be shown. Obtain permission before 1000 0 1000 2000 3000 4000 5000 6000 7000 8000 9000 10000 QUADRANGLE LOCATION entering private lands. UTM GRID AND 2016 MAGNETIC NORTH FEET DECLINATION AT CENTER OF SHEET Imagery ..................................................NAIP, June 2014 Roads................................ U.S. Cense Bureau, 2015 - 2016 U.S. National Grid CONTOUR INTERVAL 5 FEET 1 Snow Hill Names..........................................................GNIS, 2016 100,000.mSqus a ID NORTH AMERICAN VERTICAL DATUM OF 1988 1 2 3 2 Hookerton Hydrography ....................National Hydrography Dataset, 2014 3 Alden Contours............................National Elevation Dataset, 2008 TE This map was produced to conform with the 4 5 4 Falling Creek Boundaries ............ Multiple sources; see metudata file 1972 - 2016 National patial Program 5 Dn gram UST apo Product Standard, 2011. 6 Deep Run Wetlands ......... FWS National Wetlands Inventory 1977 - 2014A metadata file associated with this product Is draft version 0.6.19 6 7 8 7 Rlvermont KINSTON, NC Grid Lone o°.yR.tbR B Dover 1a5 ADJOINING QUADRANGLES 2016 `�VVVU.S. DEPARTMENT OF THE INTERIOR rhe National Map KINSTON QUADRANGLE G U.S. GEOLOGICAL SURVEY US Topo NORTH CAROLINA science for a changing world 7.5-MINUTE SERIES 77°37'30" 35' 32'30" 77°30' Z62ook E '63 264 '65_ 166 '`67- 268 270 2 440 000 FEET 272 35'22'30' -- _ - - � 35°22'30, EURANRS RD 9p ss17 4G/��0� yl 75 3B1700mN O AIRY ceoGROVE CHURCH CH RD - ha r wOOtel1S Crossroads PC � TION RD DAWSON STA 58 "OLE RUSH LN ry_ z 590000 0 175. 0tiF x -�- tea• -�- --- -- FEET I.. -ea• J.. — _.ACS..-. - "'I* R0 -11-- _ . ..-.. - y° `sib 3915 -- -� 7s 75 - - 3915 �� _ TpYLGR - Mewborns o - Crossroads m INSTITUTE RD . __ 15 _ ` s 3914 C /�, i r r C 3814 TAYLOR SPENCE RD o - �- - �V I'.�QPtNS� N 'y RD m t AMERO GSTON i Kinston Reglonal..,S. �J oERD 3 Jetport at P CNG Stallings Field J ' 1 a �.ELNORE FARMS RD —75 v_ 75 's13 0.D D /I 13 �- / H M DEAD EN R WN/TLEVDR 1--� \^ _ 0 u --- f "12 3912 z o +° m 75ngers�' E / ON991 M L p r_/00<rai CPS�PZ\ R -. -- ��-` 9q•°p� q n ^^i IE N MILL IILONMAN IL , TILGHMA 1'/ 3911 pQJ. nn n ACADEMY HEIGHTS RD l / j 835 OQg95 _ l 15 RUN ep _ ; AR '9910 1743 z BRI Y _ J I 3810. � NW ` � -z" 4 V _ a _ � S`•9$ _ 1, fP°.k}1 HODGES RD 444.< a 11 ' Poi's �\ 3 M _ _ - 11.1 7• n % �j �J I 75 INDIGO LN A A m x �f Y J O 3909 _- _ -n.. - C4REaQo RILEYRD ��XIgI,CrOq QO `� j v_.{55 '� \ 1 CRE A 0 S 1 opy �\ \ 55 5TW0p0 ORFPE° <T�pS vQ �Ps \ D°R > .� _ - o SPP R' q OP MEP m CUNN/ c EEN rz NON 1730" W Q �To�Q ° �r2 0 0 0 4MN0 . �� 1T30,� +5°gypFARM ti FOX RUN DR \ y1P ?SCC a^ OP ` 2M 3— 50 - -. -.. RD 3906 p E"Z (•P 1108 STOCKTON RD v� t / 0010 m \ O q : O Q LL W F UIf\PLAZA BLVD °O ez�o � 6 ` PARR0TT4VFDPRBY AVE x DIXON ST DONN RD c p T N II n > WILLIAMS 5T - Av CAMERON DR �_ sOM ✓ z ti w NIESTMINSTERLN oHILL ST 3907 FARM LN o ^ JOTjs m� CAVALIER CIR �- DANIELS ST o E HIGNLPNp A 1 3907 D' ¢ EE ENH NT - -_ O ,.•, h 3 a W HIGHLAND AVE �F ;0 9 �q� } p �� SPECTP .. EDWARDS AVE U W WILJ PZC Harveytown ?°�� BROWN ST -� -._..y J o z v ON J5, 11-- ` A W n W 4VF Om 55 o KINSTON A o , G_0y 15. �Hinea ✓� Bus D A - c E P r� lr q en rrRO O c SUMMIT / U a o � • m WRF _ RD/N S HOD 5 z BF `' N SRF �' V6 3 I ��!- HA G i ES AV PARK AVE A Junction UP FSr y 7 M E GRAINGER AVE :per h . N6 yI VERMO - Bus > AVE WASH/NG TON AVE Z "~' WL Bus ,L 70 m 47 , MP. lJ m�_LANTrC W W W Bus ti .ac J 3 � _ V _ Q N Rraer _ a Sg EWASHINGTONST 4 Georgetown 118 MANN/NG Sr FIELDS Si :. - W _.. _ 25� _ .� ._� LL -- -_- '_- E BLOUN7 ST T E ILL RD Oak Hilt LL. Ia 2 m i ESTNUT S7 12 CHr- ep u —' - _ E CORDON ST 'sU5 W R H -e�F y .~ V E CASWELL Sr W CASWELL ST o 05 W RD -� E KING ST ZJ CEDAR LN - - �'• ,. 11 - Z� 70 55 258 Bus Maplewood d ry�,���,. , I i - t _ ."5 Ii ti's f-. ° sY• \ ESHI \_ 1-25 X25' -- - CI N LINCOLN ST LL25 850000 ._ _...> ._ Ls- - __ bPyp° .z`' - -_ -�- _ - W 25 04 N FEET UNIVERSITY ST y - _. �. 55 70 Bus M '•zs. __. _ - 15 70 - - _ - Tj 15 �l 5 'I`- 25 35015' I,= _ _ U i 35°15' 35°t6' '62 363 26412 420 000 FEET -- '66 267 366 '69 '70 '71 '72"`-E 77°37'30" 35' 32'30" 77030' Produced by the United States Geological Survey * SCALE 1:24 000 ROAD CLASSIFICATION North American Datum of 1983 (NAD83) Expressway Local Connector Worid Geodetic System of 1984 (WGS84). Projection and 1 0.5 0 KILOMETERS 1 2 NORrR 1 000-meter grid: Universal Transverse Mercator, Zone 18S q• 4y• ROLINA A. Secondary Hwy LOcaI Road 10 000-foot ticks: North Carolina Coordinate System of 1983 172 MILS 1000 500 0 METERS 1000 2000 Ram 4WD q• 0 1 p This map is not a legal document Boundaries may be MR! generalized for this map scale. Private lands within government MILES .Interstate Route US Route O State Route reservations may not be shown. Obtain permission before 1000 0 1000 2000 3000 4000 5000 6000 7000 8000 9000 10000 QUADRANGLE LOCATION entering private lands. UTM GRID AND 2016 MAGNETIC NORTH FEET DECLINATION AT CENTER OF SHEET Imagery ..................................................NAIP, June 2014 Roads................................ U.S. Cense Bureau, 2015 - 2016 U.S. National Grid CONTOUR INTERVAL 5 FEET 1 Snow Hill Names..........................................................GNIS, 2016 100,000.mSqus a ID NORTH AMERICAN VERTICAL DATUM OF 1988 1 2 3 2 Hookerton Hydrography ....................National Hydrography Dataset, 2014 3 Alden Contours............................National Elevation Dataset, 2008 TE This map was produced to conform with the 4 5 4 Falling Creek Boundaries ............ Multiple sources; see metudata file 1972 - 2016 National patial Program 5 Dn gram UST apo Product Standard, 2011. 6 Deep Run Wetlands ......... FWS National Wetlands Inventory 1977 - 2014A metadata file associated with this product Is draft version 0.6.19 6 7 8 7 Rlvermont KINSTON, NC Grid Lone o°.yR.tbR B Dover 1a5 ADJOINING QUADRANGLES 2016 Buildings 8k Grounds, Business Office, Electric, Engineering, Environmental Services, Fleet Maintenance, Meter Reading, Stormwater, Streets, Wastewater, and Water I)aei st®ai, Abe irghk place „o Xmistop Fmblic Nemees, the mht claoim Kinston m Sf�E ff=ICATIOI S F•' PHI;Sc I ' RI RUI OO UTF LL SE'���i=R 11E1-i/AG ILI , ,�ST(Q RF F:.OSAMT8 zU'l': Ii 3I=1 BRIAN LUCAS, WATER RESOURCES MANAGER JOHN JARRELL,ENGINEER FIS L DRA �IfG-FOR RE IE R ISf�OS L 0 F R lw A! TRU TI• r�ETWW fie• zz, do 11_NST'O�N' 1'U�LJLI�C SECR'VICIES Buildings & Grounds, Business Office, Electric, Engineering, Environmental Services, Fleet Maintenance, Meter Reading, Stormwater, Streets, Wastewater, and Water Kinston, the rightplace ... AiOSE017 -'rahlic.Services9 the right ch®ice. Kinston I11 2009 a 9 SS/ <4 E 0� . GIN ;e. 91 epoega900 Ago �ppoo 42 Z?4 THE CITY OE KINSTON SEWER COL,!-ECTION SYSTEM CWSRF PROJECT NUMURR CS370527-17 RHONOA BARWICK, ®IRECTOR OE PURI -IC SERVICES STEVE MILER, P.E., ASSISTANT ®IRECTOR OF PUBEIC SERVICES BRIAN LUCAS, WATER RESOURCES MANAGER JOHN JARREL,L, P.E., CITY ENGINEER 1Fr0rimQi Dp.AW90NG.F®6'3 RMCW PUSP®SES ONLY P 22V 2617 �EC'ni e 00001 ABLE G CONTENTS �Hk S� IV IER 'UN �iUTF�LL ROW a a 'EH : HIS TATIC ® m GUN 0 SACT ®UMPUM EI�uTv SCECT90M 9 PAGES 1. Bid Advertisement. .. I go., I I I go. I a V a on. a..........................00010 1 2. Description of Work and Instructions to Bidders........ 00100 13 3, Bid Form....., I..". go. 66, a.. V*1111.1..11 "I .a d am to .... k.Abb,00330 .."..................................................00330 7 4, American Iron and Steel....................a..................00340 6 5, MBE / WBE (DBE) Compliance Statement ...1.111....... 00360 9 6. Davis Bacon Requirements ...................................00380 20 7, Bid Bond...........................................................00411 3 8, E -Verify Affidavit ..... Pon 6 ...... ...104 .............................00470 15 9, Non Collusion Affidavit .........................................00480 1 10, Equal Employment .........................:... ... ......... ..... 00490 1 11. Notice of Award .................................................. 00498 2 12. Contract............................................................00500 8 13. Notice to Proceed .................. n ................. a.......ago 00521 2 14, Performance Bond .............................................. 00611 6 15. Payment Bond ................................................... 00621 6 16. Certificate of Insurance ........................................ 00631 2 17. Attorney Certification ............................:............:. 00671 F 1 18, Financial Certification................................a....... 00672 1 19. General Conditions .................................... a........ 00700 73 20. Supplementary Conditions .................................... 00800 16 ®IVISI®B� m 1 ®GEI�IERA� C®N®I`�I®ISS SECTION # PACES 21. Summary.... ......... ......... 01010 1 22, Time Damages ................................................... 01011 1 23, Project Coordination .........:.................................. 01041 1 24. Cut and Patch .................................................... 01045 3 25, Field Engineering "."I man "I 111.skapa mop P.V Ban", 1PP1.1111111 Pa. 01050 1 26. Basis of Payment ................................................ 01150 3 27. Payment Application ............................................01152 9 28, Change Order .................................................... 01153 8 29. Meetings.......................:...................................01200 2 30. Submittals......................................................... 01300 4 31, Temporary Utilities .............................................. 01510 2 32. Barriers............................................................. 01530 2 33. Traffic............................................................... 01570 2 34. Material and Equipment ........................................01600 5 35, Contract Closeout ............................................... 01700 3 36. Cleaning...........................................................01710 2 37. Warranties and Bonds ......................................... 01740 2 i CSI ISi - SITE '�� mlry 38. Excavation Trenching of Backfilling for Pipe Lines .......02221 13 39. Waste Material Disposal...................6.......................... 02227 1 40. Erosion Control....6.......................6.......:.......................02540 6 41. Sanitary Sewer .................................................. 02560 17 47_ Sewer Repair .................................................... 02561 2 43. Clean and TV .................................................... 02562 5 44. Cured —in Place Pipe .......................................... 02565 5 45. Gravity Sewer Point Repair .... .....I II A ..................... 02568 10 46. Bypass Pumping ................................................ 02585 6 47. Manholes.......................................................... 02600 6 4S Manhole Rehabilitation ........................................ 02601 9 49. Replacement of Manholes .....: ...... ......".... .......... 02603 6 50. Pipe and Fittings.......................................................... 02700 15 51. Pipe Line Tests,. .............. ....... P ..... k .................. 02725 10 52 Access Road I...............I..I.A......10.........0............4 02850 6 53. Cast in Place Concrete .........................................03100 2 13 S TIO O!2IIIIISUP CIT OF I STO I AD 'TIS ENT FO�FIDS` did No. t�S 19-®9-9d Pursuant to Section 143-129 of the General Statutes of North Carolina, as amended, Sealed Bids will be received by the City of Kinston, North Carolina until 3:00 PH on Monday, October % 2017, at the Purchasing Coordinator's Office - In the Public Service Complex, 2360 Highway 258 South, Kinston, North Carolina 28504. Bids shall be enclosed in a sealed envelope and clearly marked on the outside of the envelope, Cid: PS IGwO947, Bids will be opened and read at 3:00 PM Monday June 12, 2017, in the Small Training Room of the City Public Service Complex at Kinston Public Service Complex, 2360 Highway 258 South, Kinston, North Carolina. lace tion .i Dido •d. 30iinch sewer , pipe. Rehabilitate p io i I 0feet of 30 inch sewer pipe ucured in place o line the old 2g5t➢4. The plans, specifications, and contract documents will be available starting February 23, 2009 for inspection at the City of Kinston Public Services Complex, at the North Carolina Offices of the Carolinas Associated General Contractors office in Charlotte and Raleigh, North Carolina and at the McGraw-Hill Construction Dodge in Raleigh, North Carolina. Complete copies of the plans, specifications and contract documents may be obtained online at www.icinstonpublicservices.com, by mail or in person from the City of Kinston Engineering Section by those qualified and who will make a bid, upon a deposit of twenty-five. dollars ($25.00) in cash or certified check (payable to the City of Kinston). The full plan deposit will be non-refundable for those contractors submitting bids. The full deposit will be returned to contractors not submitting bids provided all documents are returned in good condition at least seven (7) days prior to the bid date. Each proposal shall be accompanied by a cash deposit, cashier's check or cert ified check on some bank or trust company insured by the Federal Deposit Insurance Corporation in an amount equal to not less than 5% of the total amount of the proposal. In lieu thereof, a bid bond which conforms to the provisions of G.S. 143-129, as amended may be submitted by the bidder. Any proposal not accompanied by such deposit shall be void and will not be considered. Contractors are hereby notified that they must have the proper license under the State Laws governing their respective trades. Contractors must be licensed and general contractors must have license classification for Building Contractor. All bids will require a performance bond and a payment bond at time of contract execution (not required as part of the bid package). It is the responsibility of the bidders to insure that his/her bid is received before the hour given above. No bidder may withdraw his bid within 90 days of the date of bid opening. The right is reserved by the City to accept or reject any or all bids and to accept the bid deemed to be in the best interest of the City. For Questions contact: The City Engineer By: Tim Wood John Jarrell Purchasing Coordinator (252) 939-3239 Publication Date(s): September 3, 2017 Run 1 time: Kinston Free Press The City of Kinston is an Equal Opportunity Employer v t t1 Ali 9i I !U Ali A. COno iTUCt Road to Access Manholes 1. Road shall stabilize the Soil 2. Road shall allow water to filter through 3. Road shall have vegetation established 4. Stream crossings shall not hinder flow of water B. Line All Manholes using CIl'P Method 1. All manholes will be raised above the 100 year flood elevation. 2. Plug any leaks which may affect the curing of the liner 3. Rehabilitate the manholes using a cured in place liner C. Line 30 inch Sewer Outfall using Cured in Place Pipe. 1. After review of the Pre -construction Televised Inspecfion Sections of Pipe will be prioritized according to condition. 2. The sections of Pipe in the worst condition will be rehabilitated first. 3. 4,300 ± feet of Pipe will be rehabilitated using Cured in Place Pipe. D. Clean and Televised inspection 1. Prior to pipe lining Pipe will need to be cleaned and have televised inspection completed and reviewed by the engineer. 2. After the pipe lining has cured, a televised inspection of the pipe liner will need to be done and reviewed by the engineer. 111. � 0�I"!I �0�! 'h��I'a:�•��, N�h� Ut T I !� A. Complete sets of the Bidding Documents maybe obtained fiom the Office of the Engineer in the number and format stated in the advertisement or invitation to bid. B. Complete sets of Bidding Documents shall be used in preparing Bids; neither Owner nor Engineer assumes any responsibility for errors or rnisinterpretafions resulting from the use of incomplete sets of Bidding Documents. C. Owner and Engineer, in making copies of Bidding Documents available on the above terms, do so only for the purpose of obtaining Bids for the Work and do not authorize or confer a license for any other use. A. To demonstrate Bidder's qualifications to perform the Work, Bidder shall submit with its Bid (a) written evidence establishing its qualifications such as financial data, previous experience, and present commitments, and (b) the following additional information: Evidence of Bidder's authority to do business in the state where the Project is located. 2. Bidder's state or other conhactor license number. If Bidder is not licensed in the State of North Carolina, submit evidence of its ability to obtain a North Carolina license within the time for acceptance of Bids. 3. Subcontractor and Supplier qualification information; coordinate with provisions of Section 12 of these Instructions, "Subcontractors, Suppliers, and Others." 4. Disadvantaged Business Enterprise [DBE] Forms and Affidavits. B. A Bidder's failure to submit required qualification information with the bid will disqualify Bidder from receiving an award of the Contract. C. No requirement in this Secfion 3 to submit information will prejudice the right of Owner to seek additional pertinent information regarding Bidder's qualifications. D. Bidder is advised to carefully review those portions of the Bid Form requiring Bidder's representations and certifications. A. Site and Other Areas 1. The Site is identified in the Bidding Documents. By definition, the Site includes rights -of --way, easements, and other lands furnished by Owner for the use of the Contractor. Any additional lands required for temporary construction facilities, construction equipment, or storage of materials and equipment, and any access needed for such additional lands, are to be obtained and paid for by Contractor. 00700 - 2 B. Existing Site Conditions Subsurface and Physical Conditions; Hazardous Environmental Conditions a. Supplementary Conditions identify: i. Those reports lrnMM to Owner of explorations and tests of subsurface conditions at or adjacent to the Site. ii. Technical Data contained in such reports and drawings. b. Owner will make copies of reports and drawings referenced above available to any Bidder on request. These reports and drawings are not pari of the Contract Documents, but the Technical Data contained therein upon whose accuracy Bidder is entitled to rely, as provided in the General Conditions, has been identified and established in the Supplementary Conditions. Bidder is responsible for any interpretation or conclusion Bidder draws from any Technical Data or any other data, interpretations, opinions, or information contained in such reports or shown or indicated in such drawings. a If the Supplementary Conditions do not identify Technical Data, the default definition of Technical Data set forth in Article 1 of the General Conditions will apply. 2. Underground Facilities: Information and data shown or indicated in the Bidding Documents with respect to existing Underground Facilities at or adjacent to the Site are set forth in the Contract Documents and are based upon information and data fuuiished to Owner and Engineer by owners of such Underground Facilities, including Owner, or others. 3. Adequacy of Data: Provisions concerning responsibilities for the adequacy of data furnished to prospective Bidders with respect to subsurface conditions, other physical conditions, and Underground Facilities, and possible changes in the Bidding Documents due to differing or unanticipated subsurface or physical conditions appear in Paragraphs 5.03, 5.04, and 5.05 of the General Conditions. Provisions concerning responsibilities for the adequacy of data famished to prospective Bidders with respect to a Hazardous Environmental Condition at the Site, if any, and possible changes in the Contract Documents due to any Hazardous Environmental Condition uncovered or revealed at the Site which was not shown or indicated in the Drawings or Specifications or identified in the Contract Documents to be within the scope of the Work, appear in Paragraph 5.06 of the General Conditions. 00100 � 3 C. Site Visit and Testing by Bidders Bidder shall conduct the required Site visit during normal working hours, and shall not disturb any ongoing operations at the Site. request, and to the extent Owner has control over the Site, and schedule permitting, the Owner will provide Bidder access to the Site to conduct such additional examinations, investigations, explorations, tests, and studies as Bidder deems necessary for preparing and submitting a successful Bid. Owner will not have any obligation to grant such access if doing so is not practical because of existing operations, security or safety concerns, or restraints on Owner's authority regarding the Site. 'Bidder shall comply with all applicable Laws and Regulations regarding excavation and location of utilities, obtain all permits, and comply with all terms and conditions established by Owner or by property owners or other entities controlling the Site with respect to schedule, access, existing operations, security, liability insurance, and applicable safety programs. 4. Bidder shall fill all holes and clean up and restore the Site to its former condition upon completion of such explorations, investigations, tests, and studies. D. Owner's Safety Program: Not Used. E. Other Work at the Site 1. Reference is made to Article 8 of the Supplementary Conditions for the identification of the general nature of other work of which Owner is aware (if any) that is to be performed at the Site by Owner or others (such as utilities and other prime contractors) and relates to the Work contemplated by these Bidding Documents. If Owner is party to a written contract for such other work, then on request, Owner will provide to each Bidder access to examine such contracts (other than portions thereof related to price and other confidential matters), if any. A. It is the responsibility of each Bidder before submitting a Bid to: 1. examine and carefully study the Bidding Documents, and an y data and reference items identified in the Bidding Documents; 2. visit the Site, conduct a thorough, alert visual examination of the Site and adjacent areas, and become familiar with and satisfy itself as to the general, local, and Site conditions that may affect cost, progress, and performance of the Work; 3. become familiar with and satisfy itself as to all Laws and Regulations that may affect cost, progress, and performance of the Work; 4. carefully study all: (1) reports of explorations and tests of subsurface conditions at or adjacent to the Site and all drawings of physical conditions relating to existing surface or subsurface structures at the Site that have been identified in the Supplementary Conditions, especially with respect to Technical Data in such reports and drawings, and (2) reports and drawings relating to Hazardous Environmental Conditions, if any, at or adjacent to the Site that have been identified in the Supplementary Conditions, especially with respect to Technical Data in such reports and drawings; consider the information known to Bidder itself; information commonly known to contractors doing business in the locality of the Site; information and observations obtained from visits to the Site; the Bidding Documents; and the Site -related reports and drawings identified in the Bidding Documents, with respect to the effect of such information, observations, and documents on (1) the cost, progress, and performance ofthe Work; (2) the means, methods, techniques, sequences, and procedures of construction to be employed by Bidder; and (3) Bidder's safety precautions and programs; 6. agree, based on the information and observations referred to in the preceding paragraph, that at the time of submitting its Bid no fixrkher examinations, investigations, explorations, tests, studies, or data are necessary for the determination of its Bid for performance of the Work at the price bid and within the times required, and in accordance with the other terms and conditions of the Bidding Documents; L ecome aware of the general nature of the work to be performed by Owner and others at the Site that relates to the Work as indicated in the Bidding Documents; 8. promptly give Engineer written notice of all confl icts, errors, ambiguities, or discrepancies that Bidder discovers in the Bidding Documents and confirm that the written resolution thereof by Engineer is acceptable to Bidder; 9, determine that the Bidding Documents are generally sufficient to indicate and convey understanding of all terms and conditions for the performance and furnishing of the Work; and 00100 e 5 10. agree that the submission of a Bid will constitute an incontrovertible representation by Bidder that Bidder has complied with every requirement of this Article, that without exception the Bid and all prices in the Bid are premised upon performing and furnishing the Work required by the Bidding Documents, A. A pre -Bid conference will be held at the time and location stated in the invitation or advertisement to bid. Representatives of Owner and Engineer will be present to discuss the Project. Bidders are encouraged to attend and participate in the conference. Engineer will transmit to all prospective Bidders of record such Addenda as Engineer considers necessary in response to questions arising at the conference. Oral statements may not be relied upon and will not be binding or legally effective. �C�I�i1�Yi17�01�7�,7:�IfY:V11[I)IE.Y\c117\"1717\11171 A. All questions about the meaning or intent of the Bidding Documents are to be submitted to Engineer in writing. Interpretations or clarifications considered necessary by Engineer in response to such questions will be issued by Addenda delivered to all parties recorded as having received the Bidding Documents. Questions received less than seven days prior to the date for opening of Bids may not be answered. Only questions answered by Addenda will be binding. Oral and other interpretations or clarifications will be without legal effect. B. Addenda maybe issued to clarify, correct, supplement, or change the Bidding Documents, VIII. BID SECURITY A. A Bid must be accompanied by Bid security made payable to Owner in an amount of five percent of Bidder's maximum Bid price (determined by adding the base bid and all alternates) and in the form of a certified check, bank money order, or a Bid bond (on the form included in the Bidding Documents) issued by a surety meeting the requirements of Paragraphs 6.01 and 6.02 of the General Conditions. B. The Bid security of the apparent Successful Bidder will be retained until Owner awards the contract to such Bidder, and such Bidder has executed the Contract Documents, fiunished the required contract security, and met the other conditions of the Notice of Award, whereupon the Bid security will be released. If the Successful Bidder fails to execute and deliver the Contract Documents and furnish the required contract security within 15 days after the Notice of Award, Owner may consider Bidder to be in default, annul the Notice of Award, and the Bid security of that Bidder will be forfeited. Such forfeiture shall be Owner's exclusive remedy if Bidder defaults. 00100 = 6 C. The Bid security of other Bidders that Owner believes to have a reasonable chance of receiving the award may be retained by Owner until the earlier of seven days after the Effective Date of the Contract or 91 days after the Bid opening, whereupon Bid security furnished by such Bidders will be released. . D. Bid security of other Bidders that Owner believes do not have a reasonable chance of receiving the award will be released within seven days after the Bid opening. A. The number of days within which, or the dates Uy which, the Work is to be substantially completed, and completed and ready for final payment, are set forth in the Agreement. I I �i l lI1Di � I I IIS ID � 1�TIl/��l�llD(�� A. Provisions for liquidated damages, if any, for failure to timely attain a Milestone, Substantial Completion, or completion of the Work in readiness for final payment, are set forth in the Agreement. A. The Contract for the Work, as awarded, will be on the basis of materials and equipment specified or described in the Bidding Documents, and those "or -equal" or substitute or materials and equipment subsequently approved by Engineer prior to the submittal of Bids and identified by Addendum. No item of material or equipment will be considered by Engineer as an "or -equal" or substitute unless written request for approval has been submitted by Bidder and has been received by Engineer at least 15 days prior to the date for receipt of Bids. Each such request shall comply with the requirements of paragraphs 7.04 and 7.05 of the General Conditions. The burden of proof of the merit of the proposed item is upon Bidder. Engineer's decision of approval or disapproval of a proposed item will be final. If Engineer approves any such proposed item, such approval will be set forth in an Addendum issued to all prospective Bidders. Bidders shall not rely upon approvals made in any other manner. B. All prices that Bidder sets fort h in its Bid shall be based on the presumption that the Contractor will furnish the materials and equipment specified or described in the Bidding Documents, as supplemented by Addenda. Any assumptions regarding the possibility of post -Bid approvals of "or -equal" or substitution requests are made at Bidder's sole risk. A, A Bidder shall be prepared to retain specific Subcontractors, Suppliers, or other individuals or entities for the performance of the Work if required by the Bidding Documents (most commonly in the Specifications) to do so. If a prospective Bidder objects to retaining any such Subcontractor, Supplier, or other individual or entity, and the concern is not relieved by an Addendum, then the prospective Bidder should refrain from submitting a Bid. ]�, Subsequent to the submittal of the Bid, Owner may not require the Successful Bidder or Contractor to retain any Subcontractor, Supplier, or other individual or entity against which Contractor has reasonable objection. C. Bidders shall submit qualification statements for Contractor's or subcontractor's and equipment proposed to perform the following portions of the Work: i. As stated on the bid form. J<D. Additionally, the apparent Successful Bidder, and any other Bidder so requested, shall within five days after Bid opening, submit to Owner if requested, an experience statement with pertinent information regarding similar projects and other evidence of qualification for each other such Subcontractor, Supplier, or other individual or entity. If Owner or Engineer, after due investigation, has reasonable objection to any proposed Subcontractor, Supplier, individual, or entity, Owner may, before the Notice of Award is given, request apparent Successful Bidder to submit an acceptable substitute, in which case apparent Successful Bidder shall submit a substitute, Bidder's Bid price will be increased (or decreased) by the difference in cost occasioned by such substitution, and Owner may consider such price adjustment in evaluating Bids and making the Contract award. E. If apparent Successful Bidder declines to make any such substitution, Owner may award the Contract to the next lowest Bidder that proposes to use acceptable Subcontractors, Suppliers, or other individuals or entities. Declining to make requested substitutions will constitute grounds for forfeiture of the Bid security of any Bidder. Any Subcontractor, Supplier, individual, or entity so listed and against which Owner or Engineer makes no written objection prior to the giving of the Notice of Award will be deemed acceptable to Owner and Engineer subject to subsequent revocation of such acceptance as provided in Paragraph 7.06 of the General Conditions. 00100 - 8 A. The Bid Form is included with the Bidding. Documents. All blanks on the Bid Form shall be completed in ink and the Bid Form signed in ink. Erasures or alterations shall be initialed in ink by the person signing the Bid Form. A Bid price shall be indicated for each section, Bid item, alternate, adjustment unit price item, and unit price item listed therein. 2. If the Bid Form expressly indicates that submitting pricing on a specific alternate item is optional, and Bidder elects to not furnish pricing for such optional alternate item, then Bidder may enter the words 'No Bid" or "Not Applicable." B. A Bid by a corporation shall be executed in the corporate name by a corporate officer (whose title must appear under the signature), accompanied by evidence of authority to sign. The corporate address and state of incorporation shall be shown. The corporate seal shall be affixed and attested by the corporate secretary or an assistant corporate secretary. � C. A Bid by a partnership shall be executed in the partnership name and signed by a partner (whose title must appear under the signature), accompanied by evidence of authority to sign. The partnership's address for receiving notices shall be shown. D. A Bid by a limited liability company shall be executed in the name of the fum by a member or other authorized person and accompanied by evidence of authority to sign. The state of formation of the firm and the firm's address for receiving notices shall be shown. E. A Bid by an individual shall show the Bidder's name and address for receiving notices. F. A Bid by a joint venture shall be executed by an authorized representative of each joint venture in the manner indicated on the Bid Form. The joint venture's address for receiving notices shall be shown. G. All names shall be printed in ink below the signatures. H. The Bid shall contain an acknowledgment of receipt of all Addenda, the numbers of which shall be filled in on the Bid Form. I. Postal and e-mail addresses and telephone mmnber for communications regarding the Bid shall be shown. The Bid shall contain evidence of Bidder's authority and qualification to do business in the state where the Project is located, or Bidder shall covenant in writing to obtain such authority and qualification prior to award of the Contract and attach such covenant to the Bid. Bidder's state contractor license number, if any, shall also be shown on the Bid Form. A. Unit Price 1. Bidders shall submit a Bid on a unit price basis for each item of Work listed in the unit price section of the Bid Form. 2. The "Bid Price" (sometimes referred to as the extended price) for each unit price Bid item will be the product of the "Estimated Quantity" (which Owner or its representative has set forth in the Bid Form) for the item and the corresponding "Bid Unit Price" offered by the Bidder. The total of all unit price Bid items will be the sum of these "Bid Prices"; such total will be used by Owner for Bid comparison purposes. The final quantities and Contract Price will be determined in accordance with Paragraph 13.03 of the General Conditions. 3. Discrepancies between the multiplication of units of Work and unit prices will be resolved in favor of the unit prices. Discrepancies between the indicated sum of any column of figures and the correct sum thereof will be resolved in favor of the correct sum. 4. Allowances a. For cash allowances the Bid price shall include such amounts as the Bidder deems proper for Contractor's overhead, costs, profit, and other expenses on account of cash allowances, if any, named in the Contract Documents, in accordance with Paragraph 13.02.B of the General Conditions. III A. With each copy of the Bidding Documents, a Bidder is furnished one separate unbound copy of the Bid Form, and, if required, the Bid Bond Form. The unbound copy of the Bid Form is to be completed and submitted with the Bid security and the other documents required to be submitted under the terms of Section IX, ATTACHMENTS TO THIS BID, of the Bid Form. 00100 a 10 lE$. A Bid shall be received no later than the date and time prescribed and at the place indicated in the advertisement or invitation to bid and shall be enclosed in a plainly marked package with the Project title (and, if applicable, the designated portion of the Project for which the Bid is submitted), the name and address of Bidder, and shall be accompanied by the Bid security and other required documents. If a Bid is sent by mail or other delivery system, the sealed envelope containing the Bid shall be enclosed in a separate package plainly marked on the outside with the notation "BID ENCLOSED." A mailed Bid shall be addressed to Purchasing Manager, Finance Department, 2360 Highway 258 South, Kinston, NC 28504. (C. Bids received after the date and time prescribed for the opening of bids, or not submitted at the correct location or in the designated manner, will not be accepted and will be returned to the Bidder unopened. 1. �umll i� l�a� � m f•nmry �� � ���i l;,lm A. A Bid may be withdrawn by an appropriate document duly executed in the same manner that a Bid must be executed and delivered to the place where Bids are to be submitted prior to the date and time for the opening of Bids. Upon receipt of such notice, the unopened Bid will be returned to the Bidder. lg, If a Bidder wishes to modify its Bid prior to Bid opening, Bidder must withdraw its initial Bid in the manner specified in Paragraph 16.01 and submit a new Bid prior to the date and time for the opening of Bids. C. If within 24 hours after Bids are opened any Bidder files a duly signed written notice with Owner and promptly thereafter demonstrates to the reasonable satisfaction of Owner that there was a material and substantial mistake in the preparation of its Bid, that Bidder may withdraw its Bid, and the Bid security will be returned. Thereafter, if the Work is rebid, that Bidder will be disqualified from fiuther bidding on the Work. A. Bids will be opened at the time and place indicated in the advertisement or invitation to bid and, unless obviously non-responsive, read aloud publicly. An abstract of the amounts of the base Bids and major alternates, if any, will be made available to Bidders after the opening of Bids. A. Bids will be opened at the time and place indicated in the advertisement or invitation to bid and, unless obviously non-responsive, read aloud publicly. An abstract of the amounts of the base Bids and major alternates, if any, will be made available to Bidders after the opening of Bids, rr y- A. Owner reserves LOU right to reject any or all Bids, including without limitation, nonconforming, nonresponsive, unbalanced, or conditional Bids. Owner will reject the Bid of any Bidder that Owner fords, after reasonable inquiry and evaluation, to not be responsible. If Bidder purports to add terms or conditions to its Bid, takes exception to any provision of the Bidding Documents, or attempts to alter the contents of the Contract Documents for purposes of the Bid, then the Owner will reject the Bid as nonresponsive; provided that Owner also reserves the right to waive all minor informalities not involving price, time, or changes in the Work. B. If Owner awards the contract for the Work, such award shall be to the responsible Bidder submitting the lowest responsive Bid. C. Evaluation of Bids e. In evaluating Bids, Owner will consider whether or not the Bids comply with the prescribed requirements, and such alternates, unit prices, and other data, as may be requested in the Bid Form or prior to the Notice of Award. ano For the determination of the apparent low Bidder when unit price bids are submitted, Bids will be compared on the basis of the total of the products of the estimated quantity of each item and unit price Bid for that item, together with any lump sum items. D. In evaluating whether a Bidder is responsible, Owner will consider the qualifications of the Bidder and may consider the qualifications and experience of Subcontractors and Suppliers proposed for those portions of the Work for which the identity of Subcontractors and Suppliers must be submitted as provided in the Bidding Documents. E. Owner may conduct such investigations as Owner deems necessary to establish the responsibility, qualifications, and financial ability of Bidders and any proposed Subcontractors or Suppliers. A. Article 6 of the General Conditions, as may be modified by the Supplementary Conditions, sets forth Owner's requirements as to performance and payment bonds and insurance. When the Successful Bidder delivers the Agreement (executed by Successful Bidder) to Owner, it shall be accompanied by required bonds and insurance documentation. A, When Owner issues a Notice of Award to the Successful Bidder, it, shall be accompanied by the unexecuted counterparts of the Agreement along with the other Contract Documents as identified in the Agreement. Within 1S days thereafter, Successful Bidder shall execute and deliver the required number of counterparts of 'the Agreement (and any bonds and insurance documentation required to be delivered by the Contract Documents) to Owner. Within ten days thereafter, Owner shall deliver one fully executed counterpart of the Agreement to Successful Bidder, together with printed and electronic copies of the Contract Documents as stated in Paragraph 2.02 of the General Conditions. A, Owner is exempt from state sales and use taxes on materials and equipment to be incorporated in the Work. Refer to Paragraph SC -7.09 of the Supplementary Conditions for additional information. specs\OOIOOreselecvic 00'i00 a �3 SECTI• 00��0 �f11 1111111[111010 21 I. TH15 EIC IS SUP!��I ED l O: TIM WOOD, PURCHASING MANAGER CITY OF STr FINANCE DEPARTMENT, PURCHASING DDiVISI4 1 ��,!�� 0 Highway 260 South, Kinston, NC 2085'1 B. The undersigned BI®DEf� proposes and agrees, if this BID is accepted, to enter into an Agreement with OWNER in the form or included in the Contract Documents to complete all work as specified or indicated in the Contract Documents for the Contract Price and within the Contract Time indicated in this BID and in accordance with the Contract Documents. ll, :IDD�� � ACi 'C�L'L�DGEfi���lTS A. BIDDER accepts all terms and conditions of the General Conditions and Supplementary Conditions, including without limitation those dealing with the disposition of Bid Security. This Bid will remain open for nine days after the day of the Bid opening. BIDDER will sign the Agreement and submit the Contract Security and other documents required by the Contract Documents within five (5) days after the date of OWNER'S Notice of Award. In submitting this BID, BIDDER represents, that: A. BIDDER has examined and carefully studied the Bidding Documents, and any data and reference items identified in the Bidding Documents, and hereby acknowledges receipt of the following addenda: B. BIDDER has visited the Site, conducted a thorough, alert visual examination of the Site and adjacent areas, and become familiar with and satisfied itself as to the general, local, and Site conditions that may affect cost, progress, and performance of the Work. 00330-1 C. BIDDER is familiar with and has satisfied itself as to all Laws and Regulations that may affect cost, progress, and performance of the Work. 1. Reports of explorations and tests of subsurface conditions at or adjacent to the Site and all drawings of physical conditions relating to existing surface or subsurface structures at the Site that have been identified in the Supplementary Conditions, especially with respect to Technical Data in such reports and drawings, and 2. Reports and drawings relating to Hazardous Environmental Conditions, if any at or adjacent to the Site that have been identified in the Supplementary Conditions, especially with respect to Technical Data in such reports and drawings. 3. locality where work is to be performed, the legal requirements, (federal, state and local laws, ordinances, rules and regulations) and the conditions affecting cost, progress or performance of the Work and has made such independent investigations as BIDDER deems necessary; E. BIDDER has considered the information known to BI®DER itself; information commonly known to contractors doing business in the locality of the Site; information and observations obtained from visits to the Site; Bidding Documents; and any Site -related reports and drawings identified in the Bidding Documents, with respect to the effect of such information, observations, and documents on 1. The cost, progress, and performance of the work 2. The means, methods, techniques, sequences, and procedures of construction to be employed by BIDDER; and 3. BIDDER'S safety precautions and programs. F. BIDDER agrees, based on information the information and observations referred to in previous paragraph (III.A.5), that no further examinations, investigations, explorations, tests, studies, or data are necessary for the determination of this Bid for performance of the work at the price bid and within the times required, and in accordance with the other terms and . conditions of the Bidding Documents G. BIDDER is aware of the general nature of work to be performed by ®WNER and others at the Site that relates to the Work as indicated in the Bidding Documents. H. BIDDER has given Engineer written notice of all conflicts, errors, ambiguities, or discrepancies that BIDDER has discovered in the Bidding Documents, and confirms that the written resolution thereof by ENGINEER is acceptable to BIDDER. 00330 — 2 1. The Bidding Documents are generally sufficient to indicate and convey understanding of all terms and conditions for the performance and furnishing of the Work. J. The submission of this Bid constitutes an incontrovertible representation by BIDDER that BIDDER has complied with with every requirement of this Subsection (III), and that without exception the Bid and, all prices in the Bid are premised upon performing and furnishing the Work required by the Bidding Documents, v ei��E�s cE�TiFir-aTio�J �I®®ER certifies that: A. This bid is genuine and not made in the interest of or on behalf of any undisclosed person, firm or corporation and is not submitted in conformity with any collusive agreement or rules of any group, association, organization or corporation; B. BIDtDER has not directly or indirectly induced or solicited any other EI®DER to submit a false or sham bid; C. EI®®ER has not solicited or induced any person; firm or corporation to refrain from bidding; D. BIDDER has not engaged in corrupt, fraudulent, collusive, or coercive practices in competing for the Contract. 1.' "Corrupt practice' means the offering, giving, receiving, or soliciting of anything of value likely to influence the action of a public official in the bidding process; 2. "fraudulent practice" means intentional misrepresentation of facts made a. To influence the bidding process to the detriment of OWNER, b. To establish bid prices at artificial non-competitive levels, or c. To deprive OWNER of the benefits of free and open competition; 3. "collusive practice" means a scheme or arrangement between two or more BIDDERS,with or without the knowledge of OWNER, a purpose of which is to establish bid prices at artificial, non-competitive levels; and V. "coercive practice" means harming or threatening to harm, directly or indirectly, persons or their property to influence their participation in the bidding process or affect the execution of the Contract. 00330 — 3 I. 8011013111H A. BIDDER will complete the Work in accordance with the Contract Documents for the following price(s): lYIIJ1I/fiBER ITEM QUANTITY UNIT UNIT PRICE TOTAL 1 Temporary Access 15,000 FT, 2 Pre -construction TV Inspection 155700 FT.. 3 Point Repair on 30" Sewer 5 EA. 4 a Raise Manhole 1 foot 6 EA. 4 b Raise Manhole 2 feet 8 EA. 4 c Raise Manhole 3 feet 18 EA. 4 d Raise Manhole 4 feet 7 EA. 4 e Raise Manhole 5 feet 3 EA. 4 f Raise Manhole 6 feet 1 EA, 5 Replace Manhole Cover 4 EA. 6 a Rehabilitate Manhole (12 to 13 feet) CIPP 27 EA. 6 b Rehabilitate Manhole (13 to 14 feet) CIPP 10 EA. 6 c Rehabilitate Manhole (14 to 15 feet) CIPP 1 EA. 7 Rehabilitate 30 " Sewer CIPP 4,159 FT 8 Post Construction Televised Inspection 4,159 LS. 9 Bypass Pumping 1 LS, 10 Erosion Control ILS, 11 Mobilization 1 1 LS, 3'OTAI. ►.�i�i ti�ilrl�l� B. BIDDER acknowledges that 1. Each Bid Unit Price includes an amount considered by BIDDER to be adequate to cover Contractor's overhead and profit for each separately identified item, and 2. Estimated quantities are not guaranteed, and are solely for the purpose of comparison of Bids, and final payment for all unit price Bid items will be based on actual quantities, determined as provided in the Contract Documents. C. Bonds required under Paragraph 6.01 of the General Conditions (Section 700) will be based on the Contract Price. 00330 — 4 VIIL TIME E OF CDIV�[i PPLr.ETI[OPV A. BIDDER agrees that Work will be substantially complete within 180 calendar days after the date when the Contract Times commence to run as provided in Paragraph 4.01 of the General Conditions (Section 00700), and will be completed and ready for final payment in accordance with Paragraph 15.06 of the General Conditions (Section 00700) within 210 calendar days after the date when the Contract Times commence to run. B. M DDIER accepts the provisions of the Agreement as to liquidated damages.. VIIIIII. A'II'�'ACII3[ly1[ElOTq'S 7['® TDIIS BIID The following documents are submitted with and made a condition of this Bid: A. Required Bid Security; B. List of Proposed Subcontractors (provided in Section 00360 DBE forms Pages 00360 — 4); C. List of Proposed Suppliers of materials and equipment (Attachment A); D. Evidence of authority to do business in the state of the Project; or a written covenant to obtain such license within the time for acceptance of Bids: E. Contractor's License Number: _ F. American Iron and Steel Forms (Section 00340) G. NC Division of Water Infrastructure MBE/WBE (DBE) Compliance (Section 00360 Pages 00360 —1, 00360 —2 and 00360 - 5); H. DBE Affidavits (Section 00360 End of Section); I. EPA Form 6100-3: DBE Subcontractor Performance Form (Section 00360 Page 00360 — 4); J. BIDDER Qualifications Statement (Section 00420) 1. Schedule A (Current Experience). 2. Schedule B (Previous Experience). 3. Schedule C (Major Equipment). 4. Audited balance sheet for each of the last 3 years for firm in Section 1. 5. Evidence of authority for individuals listed in Section 7 to bind organization to an agreement. 6. Resumes of officers and key individuals (including Safety Officer of firm named in Section 1. 7. Required safety program submittals listed in Section 13, 8. Additional items as pertinent. Noncollusion Affidavit (Section 00480) L. Certification of Nonsegregated Facilities (Section 00485) M. E -Verify Affidavit (Section 00470 Page 00470 - 4) N. Iran Divestment Act (Section 00470 Page 00470 - 5) I<XX. The terms used in this Bid with Initial capital have the meanings stated in the instructions to Bidders (Section 00100), the General Conditions (Section 00700), and the Supplementary Conditions (Section 00800). 00330 — 5 By: (Signature) (Printed name) (If Bidder is a corporation, a limited liability company, a partnership, or a joint venture, attach evidence of authority to sign.) Attest: (Signature) (Printed name) Title: Submittal Date: Address for giving notices: Telephone Number: Fax Number: Contact Name and e-mail address: Bidder's License Number: Classification: Limitation: Employer's Tax ID Number: Corporation: Corporation Name: State of Incorporation: Corporate Seal: 00330-6 SE�TIO Oi�a(� AMERICAN IR®N AND S u =L QAISy Gi ii r� fo S'F ' oject� iiV tli C�.iolifI A. This state summarizes the requirements under Subsection 436 (a)(2) of the Consolidated Appropriations Act of 2014 that SRF recipients only use Iron and steel products produced in the United States. The Environmental Protection Agency provides full guidance on the requirements at the following website: http://water eDa qov/cirants funding/aisreauirernents.cfm. B. Recipients of subject SRF awards must submit the executed C�rrillf6��4I®n for SRF Projects and any waiver requests with their Bid Package. The recipient cannot receive a promissory note with out these items. C. Manufacturers can use the template "compliance Certification" fio document that materials are "produced in the United States." 1. Certification for SRF Projects 2. AIS Waiver Instruction 3. Materials covered by AIS 4. Template Compliance Certification for Materials Covered by AIS 5. Template De Minlmis list American Iron and Steel (AIS) Certification for SRF Projects ecipien s o oubjeut bmr�awards must submit this executed form and any waiver requests with their Bid Information package to State SRF program in order to receive funding. B. The (Applicant) certifies that their contractors performing construction, alteration, maintenance and repair of the public treatment works under project number will comply with subsection 436 (a)(2) of the Consolidated Appropriations Act of 2014 and only use Iron and steel products produced in the United States. Contractor (print) (sign) (date) Owner (print) (sign) (date) 00340 - 2 Ills AIS Wavier inMrucUons A. Approved national waivers can be found at this website http//water, epa, g ov/grants_funding/a i sreq u i re m e nt. cfm B. Please note that a national waiver for "de minimis" iron and steel components has been approved. A table is included in this document for use in documenting what items are to be considered as covered under this waiver. Vote that no single de minimis item can be more than I% of the total material cost of the project and the total of all de minimis items must not exceed 5% of the total material watt of the Protect. C. Waiver Requests are provided for in subsection 436(b) of the Act. It states they will be granted if the Administrator of the EPA finds that: 7. Applying subsection (a) would be inconsistenf with the public interest: 2. Iron and steel products are not produced in the United States in sufficient and reasonably available quantities and of a satisfactory quality; or 3. Inclusion of iron and steel products produced in the United States will increase the cost of the overall project by more than 25 percent. D. A checklist of items for a complete waiver application package can be found in EPA guidance document for AIS found here: http•//water epa go"rants funding/upload/AIS-final-guidance-3-20-94 pdf 9. Submit DWSRF waiver request to lfincent.tomaino a ncdenr. ov. 2. Submit CWSRF waiver request to mark.hubbard�ncdenr.gov. 3. The State will forward these to the EPA for a final determination. KINSTON, MAYOR MURPHY COUNCIL MEMBERS JOSEPH TYSON ROBERT SWINSON IV FELICIA SOLOMON SAMMY AIKEN WYNN WHITTINGTON CITY MANAGER TONY SEARS UEGEND too, attoot, tootoot RIGHT WAY«� UNDERGROUND TEUERHONE UNDERGROUND GASEMSTING SEWER It .� "w 1�'O���n�\A�'BRIERY � N. pljtl�l�"T"poor. �'� to ..of"t. 141111, ` BRIERY RUN PHASE IV M &+W M STA Io4­HW BRIERY RUN PHASE IV STA 42+M M SItA M+W BRIERY RUN PHASE IV STA 56+00 TO UA 7�0 RUN PHASE IV STA �W M STA gBoi­0 � wr�I/�. .r .�.�.,� BRIERY RUN PHASE IV STA �W M STA 112+M BRIERY RUN PHASE IV STA 112+01) TO STA 126oloW PflEPARED BY GTY OF KINSTON ENGNEERING SECTION. NOT RELEASED FOR CONSTRUCTION NOTE: LOCATION OF EXISTING UNDERGROUND UTILITIES ARE APPROXIMATE, CONTRACTOR IS REQUIRED TO CONTACT NORTH CAROLINA ONE -CALL (1-800-632-4949)72 HOURS PRIOR TO BEGINNING EXCAVATION, NOTE: PROPER WORK ZONE TRAFFIC CONTROL DEVICES SHALL BE ERECTED AND MAINTAINED IN ACCORDANCE WITH MUTCD GUIDELINES. // \\� / \ I � � ��� rrp� � � \ � 5rA I4Po \ \ � pp�� `',' �� ASC I SIA Step �l � Y ALy� �M � �.— _ rfiP (�N�IEET ��S I yu4 N � �Aw,y1� PROP BAR R m xiPpi rtE I�� � SI'IILN� � �// M M _ STA Si3S4 \ � uAxxac IePe sTA� 64 R/JSE YANHdE 4 FEFt I � �// (Et fEET ABOVE 100 YEAR ftOeO) / Y� I I I FINAL DRAWING -FOR REVIEW PURPOSES ONLY NOT RELEASED FOR CONSTRUCTION NOTES: 1. TEYPORNiT N£x.1N0 IMPACT CONSRiYC110N uAmxc sz OETNI. SI��W ` ` � _ Aii4���'1 �- _ 11P 'IPIT N����w r � _. -/ „ STA BhXI V//C Y.WHOIE 1BTA RNSE YAXHIXE a fEET (St fElT ABOVE 100 YGR PLOW) RwAelurATE YAxxau: ``'�,/' usE aRm iH Pu¢ uxPx c �A 11�a, lbw I \ kRE� ILWo) E LHpl Im�ii��i1'i'�1f'iii`iii����������������■■����������������i■������������������i.���m Q�.'1 alex 0 a �Un N W O oa w Z w Q f Z �— � O ci N d t� i Z � � � � � Y w � x U ? Q � W m W (� Z 1f1 � � w N� U a M ''. F— O U O W � � � O W � � �- >_ H Z z W � � O (/) O D' t- Q � � ~ a o � J "f' LLJ mQ O � = a m W F- � � �� � � �_- � ��� ��� �� _ �''n 'II � ��� SHEET NO. 2 OF�4_ SHEETS KINSTON, MAYOR MURPHY COUNCIL MEMBERS JOSEPH TYSON ROBERT SWINSON IV FELICIA SOLOMON SAMMY AIKEN WYNN WHITTINGTON CITY MANAGER TONY SEARS UEGEND too, attoot, tootoot RIGHT WAY«� UNDERGROUND TEUERHONE UNDERGROUND GASEMSTING SEWER It .� "w 1�'O���n�\A�'BRIERY � N. pljtl�l�"T"poor. �'� to ..of"t. 141111, ` BRIERY RUN PHASE IV M &+W M STA Io4­HW BRIERY RUN PHASE IV STA 42+M M SItA M+W BRIERY RUN PHASE IV STA 56+00 TO UA 7�0 RUN PHASE IV STA �W M STA gBoi­0 � wr�I/�. .r .�.�.,� BRIERY RUN PHASE IV STA �W M STA 112+M BRIERY RUN PHASE IV STA 112+01) TO STA 126oloW PflEPARED BY GTY OF KINSTON ENGNEERING SECTION. NOT RELEASED FOR CONSTRUCTION NOTE: LOCATION OF EXISTING UNDERGROUND UTILITIES ARE APPROXIMATE, CONTRACTOR IS REQUIRED TO CONTACT NORTH CAROLINA ONE -CALL (1-800-632-4949)72 HOURS PRIOR TO BEGINNING EXCAVATION, NOTE: PROPER WORK ZONE TRAFFIC CONTROL DEVICES SHALL BE ERECTED AND MAINTAINED IN ACCORDANCE WITH MUTCD GUIDELINES. // \\� / \ I � � ��� rrp� � � \ � 5rA I4Po \ \ � pp�� `',' �� ASC I SIA Step �l � Y ALy� �M � �.— _ rfiP (�N�IEET ��S I yu4 N � �Aw,y1� PROP BAR R m xiPpi rtE I�� � SI'IILN� � �// M M _ STA Si3S4 \ � uAxxac IePe sTA� 64 R/JSE YANHdE 4 FEFt I � �// (Et fEET ABOVE 100 YEAR ftOeO) / Y� I I I FINAL DRAWING -FOR REVIEW PURPOSES ONLY NOT RELEASED FOR CONSTRUCTION NOTES: 1. TEYPORNiT N£x.1N0 IMPACT CONSRiYC110N uAmxc sz OETNI. SI��W ` ` � _ Aii4���'1 �- _ 11P 'IPIT N����w r � _. -/ „ STA BhXI V//C Y.WHOIE 1BTA RNSE YAXHIXE a fEET (St fElT ABOVE 100 YGR PLOW) RwAelurATE YAxxau: ``'�,/' usE aRm iH Pu¢ uxPx c �A 11�a, lbw I \ kRE� ILWo) E LHpl Im�ii��i1'i'�1f'iii`iii����������������■■����������������i■������������������i.���m Q�.'1 alex 0 a �Un N W O oa w Z w Q f Z �— � O ci N d t� i Z � � � � � Y w � x U ? Q � W m W (� Z 1f1 � � w N� U a M ''. F— O U O W � � � O W � � �- >_ H Z z W � � O (/) O D' t- Q � � ~ a o � J "f' LLJ mQ O � = a m W F- � � �� � � �_- � ��� ��� �� _ �''n 'II � ��� SHEET NO. 2 OF�4_ SHEETS G ne z nEr � ioo iErn P E xANNCIE IN PLACE xNFA � \ \ \ � ``',(/, c � \ \ \� � � �\ „-� ',� \` NOTES: L. mLPaxNLv xEnwvo ixPAer coxsmucnax xxmxo sEE CElNL �4i'g FINAL DRAWING -FOR REVIEW PURPOSES ONLY NOT RELEASED FOR CONSTRUCTION /�-- '^ o / oa rc / � D � m / d h z a � Z W �'h Oi Z � O ti N ,moi \ �_ E � Z W = o �c o 0 SN,> � Y W � Y U ? YusT„A��v�sse a Li j � ryANg � 10 `�/', O � W N x�g i�� LCb � �(/. 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J33B II1I g � SIA MIDJ `l`/C SIA IgIT1l � W A �n..0 A, as+oo _1 NOTES: FINAL DRAWING—fOR REVIEW PURPOSES ONLY +. aDsvxc (n> 5IA nNSDJ ro STA 3sIw5 �� NOT RELEASED FOR CONSTRUCTION TEMPORARY CSOSYNC IMPACT Cd+51S11CFiDN wrnxc sEE DEan z TEUFaawr BOFFER DIPACT (e) wxsFRucncx uArnxO ZDNE 1 STA 3Hn01 TD STA SMSD.J IND STA 65f053 ro STA SS+SSS LNlE 2 STA SH10A TD STA 5He0.J AND SIA W]55 TC STA 55!35,5 ] IEYPORARY YfltAND IMPACT CONSRYIC+Ip! g YAl11HG SFE DETAR 1 ;� A °, FFEF��W�� -- � n3� ao' w � _ '(C L `�� +°^ TEAR n�� � o Z w � 0 � Z N E-- � 0 U Z w = o ��sn Y W � x U Z Li j � p oc w '^ W eD y Z N �, U yf J W s (,� m o a /�' � o � o U + W �'-) � O � W � Q N �� � Z � O � OF � i= a a=o � H- d o � � + W m � � a m W H � � SHEET NO. 5 OF�a_SHEETS �� o g � ��� � a SHEET NO. 5 OF�a_SHEETS NOTES: 1. CR(XMNG (2) BTA. 68101.7 N STA. 60411.8 ). CROSSNG f61 GTA. 5040).2 TO WA. %45.0 TF31PORMY CROSBNG IMPACT CONSTRUCTION Y m YNO IMPACT CONSTRUCTION MATTW SEE DETAIL gEdi0S9uK 2 TEMNNARY BUFFER IMPACT (2) COHSIRUCTON MATTING 5 TEMPORARY BUTFR IMPACT (5) OOiSIRUCTOf MATTO ZONE 1 STA. 68451.7 TO STA 68401.7 AND STA 6"11.8 TO STA. W" d ZONE i STA 58461.0 TO STA. 50107.2 AND SM 60+20.0 M STA. 3"751 ZONE 2 STA 63441.7 TO BTA. 68461.7 AND STA. 6"45S TO STA. 6"70.4 ME 2 STA, SB+31.7 T1 STA 5"61.0 MD SM 5"752 W STA. 6"054 J. CROS9N0 (3) WA GB+W.B M WA 65+07.6 0. 1F16PORMY I ETANO IMPACT CONSTNCTON TEMPO6ARY CHUMMING IMPACT CONSIRIICiIdN MATINO SEE MAIL MATTING SCE MAL A TTGNPNARY sOFER IMPACT (J) COlSW 011 YATTOG ME 1 WA 65+57.8 TO WA S"W.6 AND WA 651W.B TO WA 661]7.6 SNE 2 STA 65137.8 W BTA 65+57.8 AND STA IMI+V8 M WA 6"47.8 5 CRC STNO (4) WA 6 V.8 M WA 04+SA2 TEMPORARY CROWING NPACT CdiSTRIICTOI MATTING SEE DETAIL G. TEMPORARY WFFER IMPACT (4) CONSIRIICTON MATTING ZONE 1 STA 63+057 M STA WV48 AND STA 6"352 TO WA 6 69.3 ZONE 2 WA 6J+750 M STA 63406.7 AND WA BM60.3 M WA 6N051 eov 7EEr s ed' 06• w `M'he;(R AIA} TZS A Ta%2�"I1{6�.'w \'Ew S 7'ro 29� SA412407 02 'do / / WA 01+71 MMHOE 1706 flAISE MMNOE J ]FET (2+ iEET ABOVE 100 TEAR fiAW) RdA61MAW MANHOE SE "REB IN PLACE MINER �!\/ FINAL DRAWING -FOR REVIEW PURPOSES ONLY NOT RELEASED FOR CONSTRUCTION •� 2 O 12 eo•11a � F STke111�(21 O N ��6A5 K N3N m € $ 66 £ g SHEET N0. 6 OF�.�SHEETS - I, FINAL DRAWING -FOR REVIEW PURPOSES ONLY NOT RELEASED FOR CONSTRUCTION NOTES: 1. IFMPCpMY MflLWD IMPACT NN511NIC11IX! 4ATiINO SEE DETAIL S x DEpi Sky aCt YWiccT,�tFEDm `C Ir FTro r \ STA ED✓+xaTnM` Ito AlOy� \ MANMEE V Di FEET �n�oFm � `1a/ — — — rtu+� me � i rr/a rt°°ul y4 `C mmoiX `�/� � mumu`" nAa o I�■■■�r'��■III■■I����■■■■■■■■■■■i���r'i��ii■■■■■���■■■■■■■■��■�!�L�I�!■■■■■s■■■■■� ■■■■■Ci■III■■I■■r0=.LCL■■■■■■=I==■■■■■■:I'J=S5■■■��lI�II■■■:�■■■■■■■■■■■■ SHEET N0. 7 OF�L SHEETS mai SHEET N0. 7 OF�L SHEETS 910 SHEET N0. 7 OF�L SHEETS r sTA o»azT °P°'�n 4NiHOLE B)D PNff YANNOLE S RET '� 0 � CRY A M `� CORS IN PUCE UNFA FLODJ) �Y � S >1P �. A + gCi �� M 4� po //—_ \� � � �� M+ � / / � \ \ \ ` � � >'' � ���\ J'��� M ;fix � � / / � yA / / `� � `1//. �� / � `� / .(�j w / `F s / ,/„ � `�(� ,lyp1� 9 � fad 5TA 07+526 `C MANXIXE B)D STA BM)S.S / PNff YNRIOU: i fWT \ / / (Z+ {FET ABDVE 100 YEAR RW'U) MANNOIE 6R � � PENAPoUTATE YANHOIE \PNff YANHOIf 4 RET / / Uff CUPED IN PIACE UNFR (x+ RET APove im YFAR RNoo) RFHABIUTATE YAHHOU: DISE WREO IN IMR UNEA / /``'(,/'� � \ —� ' c c \ III I I 1. FINAL DRAWING -FOR REVIEW PURPOSES ONLY NOT RELEASED FOR CONSTRUCTION t. iFbPORARY YkMVD IMPACT CONSIPIICTON uAmxc ffE oSTNL NOTES: 96+00 97+00 ~ O Z W � Q � Z ~ a � Z w � c 0 0 � Y W � Y U ? 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MOMNO (1) STA 110+652 HI Vol. 111+20.1 O W (= Op IIME MMXDIE 4IFFY TENPpfMY CROS9XC IMPACT CWSIPIIC11pN (n Z W I2+ FEET mW 100 YEAR fL000) 'FEkI0 S¢ DEM. lV J,, USE WREO M PUCE UNFA 2 ME TEIIPWWAaFTER11M66R M STA 11" MD STA 1101+20.1 TD STA I11+58.I ~ J 14A ME S STA 110+1&] M WX 110 I1.2 M111+58.1& 111+58.1 M STA 111+70.1 m O 1ELPDRMY w D IYPAU CCNSIRUMM N MATPNO ME INIM. d N 4;06� ■tea■lii■i■■■■■iii■■■i■■■■■■■■111■■■■■S■Qi■■■� ' . 1. ■■■■■■■■■111■■■■■■111■■�■■■111■■■■■■II■■■■■■■■■■■■■111■■■■■���■■■■ :. ■�■■■■■■■11�■■■■■■111■■■���11�������11��������������1���=====■■■�� ' ---------- ��� SHEET NO. 9 OF��SHEETS (x+ EEEf ABOVE IDO TENT flDOD) arae xal�q. 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