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HomeMy WebLinkAboutNC0085812_SOC (application)_20200109 Union County, NC Grassy Branch Wastewater Treatment Plant NPDES Permit No. NC0085812 RECEIVED Ow` C O& JAN 0 g 2020 1842; r A NCDEQ/DWR/NPDES J � * C. ► 4°/4•"'�'h D p RUC' \/ ry CA go Application for Special Order by Consent December 2019 Union County 500 N Main St Monroe NC 28112 Union C_ ounty Gover . T. 704-283-3500 www.unioncountync.gov L:S 1. 1842 December 30, 2019 RECEIVED Ms. Julie Grzyb JAN 09 1020 Supervisor, Complex Permitting Unit N.C. Department of Environmental Quality NCDEQ/DWR/NPDES Division of Water Resources, Water Quality Section 1617 Mail Service Center Raleigh, NC 27699-1617 RE: Union County Public Works —Grassy Branch Wastewater Treatment Plant NPDES Permit No. NC0085812 Application for Special Order by Consent Dear Ms. Grzyb, We have enclosed one original and two copies of the completed and executed application form and required attachments for a Special Order by Consent (SOC) for the Grassy Branch Wastewater Treatment Plant (WVVTP), National Pollutant Discharge Elimination System (NPDES) Permit NC0085812. We have enclosed the following documents: 1. Application for SOC to include the following attachments: a. Attachment III —Additional Flow or Flow Reallocation b. Attachment IV— Necessity Narrative c. Attachment V— Engineer's Certification d. Attachment VI — Predicted Compliance Schedule e. Attachment VII — Fund Sources Identification 2. SOC Pre-Application Certification 3. Non-refundable $400 fee The County has worked diligently to manage the potential for compliance issues at the Grassy Branch VVWTP. We have been actively involved in reduction of infiltration and inflow (I&I) in the collection system and we continue to operate and maintain the Grassy Branch WWTP to the best of our ability with the existing infrastructure. We believe that the majority of the Notice of Violations (NOVs) are attributed to record rainfall in the region. However, we acknowledge that over-allocation of sewer connections to the Grassy Branch VVWTP has contributed to and intensified the compliance issues. Therefore, we respectfully request a permanent additional flow allocation as part of the SOC. Our engineer, Hazen and Sawyer, recommends a permanent coo p . 1842 ie. increase in the design maximum month flow from 0.05 mgd to 0.120 mgd. We appreciate the time and effort of the NPDES Complex Permitting Unit to review our application for the SOC. Please do not hesitate to contact us if you have any questions. Sincerely, William M. Watson, County Manager Enclosures cc: Corey Basinger, DWR Regional Office, Water Resources Supervisor Andrew Neff, PE, Union County Public Works, Water and Wastewater Division Director Scott Honeycutt, Engineering Director John Shutak, CIP Manager Hyong Yi, Union County Public Works, Public Works Administrator Jim Struve, PE, Hazen and Sawyer Bart Farmer, Water reclamation Superintendent 04 Coo Page 2 rH CARO Union County, NC Grassy Branch WWTP NPDES Permit No. NC0085812 Application for Special Order by Consent Table of Contents Tab A. Application Form for Special Order by Consent(SOC) Tab B. Attachment III -Additional Flow or Flow Reallocation Tab C. Attachment IV- Necessity Narrative Tab D. Attachment V- Engineer's Certification i. Attachment A—Crooked Creek QUAL2K Model Development(Tetra Tech) ii. Attachment B—Crooked Creek QUAL2K Model Application for Grassy Branch WWTP (Tetra Tech) Tab E. Attachment VI - Predicted Compliance Schedule Tab F. Attachment VII - Funding Sources Identification Tab G. SOC Pre-Application Certification STATE OF NORTH CAROLINA DEPARTMENT OF ENVIRONMENT AND NATURAL RESOURCES DIVISION OF WATER RESOURCES APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) I. PERMIT RELATED INFORMATION: 1. Applicant (corporation,co oration, individual, or other): Union County Public Works pp 2. Print or Type Owner's or Signing Official's Name and Title: William M. Watson, County Manager i GrassyBranch Wastewater Treatment Plant 3. FacilityName (as shown on Permit):. ) 4. Owner Phone: 704-283-3636 (or) 5. Owner Email: Mark.Watson( ,unioncountync.gov R E C;F I V E D 4. Application Date: June 28, 2019 JAN 0 9 1010 5. NPDES Permit No. (if applicable): NC0085812 NCDEQ/DWR/NPDES 6. Name of the specific wastewater treatment facility (if different from 1.3. above): Same II. PRE-APPLICATION MEETING: Prior to submitting this completed application form, applicants must meet with the appropriate regional office staff to discuss whether or not an SOC is appropriate for this situation. Please note the date this meeting occurred and who represented the permittee: Representative: Corey Basinger Date: May 2, 2019 III. ADDITIONAL FLOW OR FLOW REALLOCATION: In accordance with NCGS 143-215.67(b), only facilities owned by a unit of government may request additional flow. Refer to Attachment III Additional flow may be allowed under an SOC only in specific circumstances. These circumstances may include eliminating discharges that are not compliant with an NPDES or Non-discharge permit. These circumstances do not include failure to perform proper maintenance of treatment systems, collection systems or disposal systems. When requesting additional flow, the facility must include its justification and supporting documentation. If the requested additional flow is non-domestic, the facilitymust be able to demonstrate the q ability to effectively treat the waste and dispose of residuals. The applicant must provide a detailed analysis of the constituents in the proposed non-domestic wastewater. The total domestic additional flow requested: 120,000 gallons per day. The total non-domestic additional flow requested: 0 gallons per day. The total additional flow(sum of the above): 120,000 gallons per day. Please attach a detailed description or project listing of the proposed allocation for additional flow, with an explanation of how flow quantities were estimated. Further, any additional flow requested must be justified by a complete analysis, by the permittee, that additional flow will not adversely impact wastewater collection/treatment facilities or surface waters. IV. NECESSITY NARRATIVE: Please attach a narrative providing a detailed explanation of the circumstances retarding the necessity of the proposed SOC. Include the following issues: Refer to Attachment IV • Existing and/or unavoidable future violations(s) of permit conditions or limits(s), • The existing treatment process and any process modifications that have been made to date to ensure optimum performance of existing facilities, • Collection system rehabilitation work completed or scheduled (including dates), • Coordination with industrial users regarding their discharges or pretreatment facilities. Identify any non-compliant significant industrial users and measure(s) proposed or already taken to bring the pretreatment facilities back into compliance. If any industrial facilities are currently under consent agreements, please attach these agreements, • Date and outcome of last Industrial Waste Survey, • Whether or not the facility is acting as a regional facility receiving wastewater from other municipalities having independent pretreatment programs. V. CERTIFICATION: The applicant must submit a report prepared by an independent professional with expertise in wastewater treatment. This report must address the following: Refer to Attachment V • An evaluation of existing treatment units, operational procedures and recommendations as to how the efficiencies of these facilities can be maximized. The person in charge of such evaluation must sign this document. • A certification that these facilities could not be operated in a manner that would achieve compliance with final permit limits. The person making such determination must sign this certification. • The effluent limits that the facility could be expected to meet if operated at their maximum efficiency during the term of the requested SOC (be sure to consider interim construction phases). • Any other actions taken to correct problems prior to requesting the SOC. 2 VI. PREDICTED COMPLIANCE SCHEDULE: The applicant must submit a detailed listing of activities along with time frames that are necessary to bring the facility into compliance. This schedule should include milestone dates for beginning construction, ending construction, and achieving final compliance at a minimum. In determining the milestone dates, the following should be considered: Refer to Attachment VI • Time for submitting plans, specifications and appropriate engineering reports to DWR for review and approval. • Occurrence of major construction activities that are likely to affect facility performance (units out of service, diversion of flows, etc.)to include a plan of action to minimize impacts to surface waters. • Infiltration/Inflow work, if necessary. • Industrial users achieving compliance with their pretreatment permits if applicable. • Toxicity Reduction Evaluations (TRE), if necessary. VII. FUNDING SOURCES IDENTIFICATION: The applicant must list the sources of funds utilized to complete the work needed to bring the facility into compliance. Possible funding sources include but are not limited to loan commitments, bonds, letters of credit, block grants and cash reserves. The applicant must show that the funds are available, or can be secured in time to meet the schedule outlined as part of this application. Refer to Attachment VII If funding is not available at the beginning of the SOC process, the permittee must submit a copy of all funding applications to ensure that all efforts are being made to secure such funds. Note: A copy of the application should be sufficient to demonstrate timeliness unless regional office has reason to request all information associated with securing funding. THE DIVISION OF WATER RESOURCES WILL NOT ACCEPT THIS APPLICATION PACKAGE UNLESS ALL OF THE APPLICABLE ITEMS ARE INCLUDED WITH THE SUBMITTAL. Required Items: a. One original and two copies of the completed and appropriately executed application form, along with all required attachments. • If the SOC is for a City / Town, the person signing the SOC must be a ranking elected official or other duly authorized employee. • If the SOC is for a Corporation / Company / Industry / Other, the person signing the SOC must be a executive officer of at least the level of vice- president, principal president, or his duly authorized representative. • If the SOC is for a School District, the person signing the SOC must be the Superintendent of Schools or other duly authorized employee. 3 Note: Reference to signatory requirements in SOCs may be found in the North Carolina Administrative Code [T15A NCAC 2H .1206(a)(3)]. b. The non-refundable Special Order by Consent (SOC) processing fee of$400.00. A check must be made payable to The Department of Environment and Natural Resources. c. An evaluation report prepared by an independent consultant with expertise in wastewater. (in triplicate) APPLICANT'S CERTIFICATION: (NO MODIFICATION TO THIS CERTIFICATION IS ACCEPTABLE) I, / /I' '4-14414'1 /Y . �i�l S�✓� , attest this application for a Special Order pp p by Consent (SOC) has been reviewed by me and is accurate and complete to the best of my knowledge. I understand if all required parts of this application are not completed and if all required supporting information and attachments are not included, this application package may be returned as incomplete. (Please be advised that the return of this application does not prevent DWR from collecting all outstanding penalties upon request). Furthermore, I attest by my signature that I fully understand that an upfront penalty, which may satisfy as a full settlement of outstanding violations, may be imposed. {Note: Reference to upfront penalties in Special Orders by Consent may be found in the North Carolina Administrative Code [T15A NCAC 2H .1206(c)(3)].} .67 Date 2 30 20 Signature o Signing Official William M. Watson, County Manager Printed Name of Signing Official THE COMPLETED APPLICATION PACKAGE, INCLUDING THE ORIGINAL AND TWO COPIES OF ALL SUPPORTING INFORMATION AND MATERIALS, SHOULD BE SENT TO THE FOLLOWING ADDRESS: NORTH CAROLINA DIVISION OF WATER RESOURCESRECEIVED POINT SOURCE BRANCH JAN 0 9 2020 1617 MAIL SERVICE CENTER RALEIGH,NORTH CAROLINA 27699-1617 NCDEQIDWRINPDES IF THIS APPLICATION IS FOR A NON-DISCHARGE SYSTEM, THEN SEND TO: NORTH CAROLINA DIVISION OF WATER QUALITY AQUIFER PROTECTION SECTION 1636 MAIL SERVICE CENTER RALEIGH,NORTH CAROLINA 27699-1636 4 STATE OF NORTH CAROLINA DEPARTMENT OF ENVIRONMENTAL QUALITY DIVISION OF WATER RESOURES APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT III. Additional Flow or Flow Reallocation 1. Background Union County owns and operates the Grassy Branch VWVTP and associated collection system infrastructure. The WWTP is permitted to discharge 0.05 mgd of treated effluent into Crooked Creek via NPDES permit NC0085812. The collection system consists of approximately 31,000 feet of gravity sewer, 123 manholes, and two wastewater pump stations. The Loxdale Pump Station pumps 21,400 gpd and the Unionville Pump Station pumps 10,245 gpd. The Grassy Branch WWTP receives only domestic wastewater. The VUVVTP serves three schools, two residential subdivisions, and several private parcels, summarized as follows: • Piedmont High School (1,363 students) • Piedmont Middle School (1,018 students) • Unionville Elementary School (701 students) • Loxdale Subdivision (52 homes) • Smithfield Subdivision (62 homes) • Private parcels (12 homes) 2. Summary of Flow Issues The County has received Notice of Violations (NOVs) for flow, five-day biochemical oxygen demand (BOD5), ammonia (NH3-N), fecal coliform, total suspended solids (TSS), and pH over the last several years. The Grassy Branch WWTP NOVs are summarized in Table III-1. The County has attributed the majority of the NOVs to record rainfall events in the region; however, over-allocation of sewer connections to the Grassy Branch WWTP has contributed to and intensified the compliance issues (refer to Section 5 of this attachment). Figure III-1 provides an illustration of the Grassy Branch VVVVTP flow and recorded rainfall. The data demonstrates that the design flow capacity is exceeded during rain events. Influent flow peaks have exceeded a ratio of 7 to 1 (e.g., peaking factors greater than 7) compared to the design capacity of the WWTP. Additionally, record rainfall was recorded in the region in 2018 through May 2019. Figure III-2 provides the monthly rainfall in the region from January 2015 through August 2019. The average monthly rainfall in the region is approximately four inches. APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT III. Additional Flow or Flow Reallocation Table III-1: Summaryof Notice of Violations for GrassyBranch WWTP Permit Violation Flow BOD5 BOD5 NH3-N NH3-N TSS (monthly (weekly (monthly (weekly (monthly Fecal (weekly Date average) average) average) average) average) Coliform average) pH 1/31/2018 0.058 2/3/2018 23 1,500 2/28/2018 0.07 220 3/3/2018 6,971 3/17/2018 3/31/2018 27.1 3/31/2018 20.3 16.3 6/2/2018 13.2 2,949 10/6/2018 440 10/13/2018 570 10/20/2018 810 10/31/2018 0.056 11/10/2018 1,200 11/17/2018 6,000 11/30/2018 0.088 12/11/2018 9.97 12/15/2018 7,200 12/22/2018 16.1 560 12/29/2018 17 6,000 12/31/2018 0.106 4.86 1,448 1/5/2019 737 1/12/2019 23.3 1/31/2019 0.10 2/28/2019 0.07 4/6/2019 193 6,000 177 4/13/2019 14.6 6.05 4/30/2019 0.065 24.8 2.05 Page 2/10 APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT III. Additional Flow or Flow Reallocation 0.35 — - 6 - 0 0.30 — ♦ 0 - 5 0 - 0 0.25 — o 0 % - 4 0 0 0.20 —73 o E - .1 O ®• ° O 0 .c 0 0 3 4pw 0 ® 0 LT 0.15 - 0 0 °� ° o — - • ♦ 0 8 •• 00 0 00 cc � O . 0 • 8 0 •• _ 0 0 0 0 0 p 8 ♦ - ♦ p4 °0 - 2 - •• 0 0 0 o 0 0 4 • , • • 0 o 8 • 0.10 - 0 0 ;oo 0o 00 o o • o , .I.i 11 Q • " 0 1 :Mir 1 • -,4".. .. ;1 aNc. 0 , • .... . : I ',Go 8 .4.i., 0 . .. ; z,l'--4.i.x"-). ., ,,. , - i _ ,.,,.04 0..1: ^ i - _' •,' •. • w. it•P. ‘0 ..;,,t t•I'l-.• s 104:1.41...A.•.--Ni.1111 II i'V �. +� y. •: •• a 1 .,"• r: . • . I' • �'i _ P. . • :SR • � �,• � �i�'' 10 eau 0.00 ti . . . r . . . ti . . . . �►. . , . r . . . . . . . , 0 Jan-15 Jul-15 Jan-16 Jul-16 Jan-17 Jul-17 Jan-18 Jul-18 Jan-19 Jul-19 Jan-20 —Design Flow 0 Flow — —Rain Fall —30-day Inf. Flow Mov. Avg Figure III-1: Grassy Branch VVWTP Influent Flow and Daily Rainfall Page 3/10 APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT III. Additional Flow or Flow Reallocation 12 — •Rain 10 — �, 8 — a) - 0 - C 6 — (13 4 c o : 1 . I II L L CC03 ) E E D (1' 2 ' E E = cn 2 ' E E D (D 2 ' E E D cB 2 ' E E c a) a) c a) aD c a) a) c a) a) c 2 a) CD Z CO Z Z z z 2015 2016 2017 2018 2019 Figure III-2: Regional Monthly Rainfall from January 2015 through August 2019 Page 4/10 APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT III.Additional Flow or Flow Reallocation 3. Summary of Infiltration and inflow (I8,1) Reduction Efforts The County has actively been involved in the reduction of infiltration and inflow (I&I) in the collection system. A Phase 1 I&I study was commissioned in 2016 to broadly determine problem areas. A Phase 2 study in 2017 focused on repair efforts readily identified in the Phase 1 study. The Phase 2 study also included wet weather monitoring. In 2018, Phase 3 efforts included confirming the effectiveness of previous repair efforts, extensive closed-circuit television (CCTV) review of the entire collection system, and the continuation of repair efforts. Phase 4 of the I&I reduction effort was initiated in January 2019. This phase consists of a review of dry and wet weather data and patterns and on-going inspection of the collection system. As of January 2019, the entire Grassy Branch collection system has been surveyed by CCTV. As of May 2019, 42 manholes have been grouted and 48 inflow collectors installed. Table III-2 provides a summary of the maintenance data for the l&I reduction effort from 2014 to present, including investigative man hours and quantity of repaired infrastructure (e.g., manholes, laterals, etc.). Table I11-3 provides a detailed summary and timeline of the County's l&l reduction efforts. Table III-2: Summary of l&I Effort Maintenance Data 2014 2015 2016 2017 2018 2019 Man Hours Investigating 960 1080 960 480 1512 1152 Man Hours Repairing 360 48 0 72 1152 192 Footage Cleaned 0 0 10,181 425 10,146 CCTV Footage 160 40 10,181 160 16,273 14,627 Hours Smoke Testing 24 20 36 36 37 32 Smoke Test Footage 14,745 7,283 4,235 4,570 15,308 8,368 Manholes Repaired 3 0 0 0 42 3 Lateral Repaired 6 4 0 4 25 8 Cleanouts Repaired 6 4 0 4 17 8 Inflow Dishes Installed 0 0 0 0 53 0 APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT III. Additional Flow or Flow Reallocation Table III-3: Grassy Branch WWTP Basin Detailed l&l Abatement Timeline March 2016— Flow monitoring conducted by Frazier Engineering (90 day study) • Identified 5 key locations within the trunk sewer to install AN flow meters. • Meters removed June 2016. June 2016—Results from flow monitoring study delivered • Identified significant I&I in upstream private system from Piedmont Middle and High school campuses. September 2016— Issued NOV to Union County Public Schools (UCPS)for violation of the UCPW Sewer Use Ordinance • NOV issued a 90 day deadline to repair deficiencies; no response. • January 3, 2017—Issued follow-up correspondence to UCPS. • January 6, 2017—UCPS issues statement of repair completion by January 17. • January 26, 2017—UCPS declares work is complete and UCPW may re-inspect. • February 27, 2017 and March 22, 2017—Issued correspondence to inform UCPS of outstanding repairs identified during smoke test re-inspection. UCPS declared that funding was not available during their fiscal year but that funds were identified the following FY with a project specifically designed for I&I abatement per the NOV. • July 18, 2017—UCPS issued Notice to Proceed to their contractor with completion date of August 2017. • August 9,2017—UCPW and UCPS conducted post-smoke test re-inspection. Found a number of deficiencies • still exist.August 14,2017—Re-inspection showed all repairs had been made satisfactorily. October 2017— Phase 2 Flow Monitoring—Follow-up (90 day study) • Frazier Engineering installed 5 AN flow meters in exact locations from previous study to determine effectiveness of repairs and identify other areas requiring attention. • Meters removed January 2018. February 2018— Results from flow monitoring study delivered • Identified other significant I&I areas in the trunk sewer upstream of the WWTP. April 2018— Began in-house I&I efforts based on flow monitoring results • Conducted I&I search during numerous late night rain events. Plugged line segments between manholes to identify I&I entry points. o Any line segment identified as an I&I entry point was inspected via CCTV. • CCTV inspection identified a defective tap which was repaired. • Repair was made and re-inspected via CCTV to affirm the repair. • Conducted 35 manhole inspections from GB WWTP to Smithfield subdivision connection. o Identified 5 manholes with defects. o All manholes repaired utilizing chemical grout injection, hydraulic cement, and ring/cover and inflow dishes where needed. May 2018— Flow monitoring follow up— Frazier Engineering (90 day study) • Monitor area limited to"micro-monitor" most significant contributor of I&I determined by previous study. May 2018 -- I&I efforts in branch sewers in Loxdale and Smithfield subdivision • Efforts include smoke tests, MH inspections, and CCTV all services and connections. APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT Ill. Additional Flow or Flow Reallocation Table III-3: Grassy Branch WWTP Basin Detailed 18,1 Abatement Timeline o Loxdale area • 3 manholes were identified for repairs—Repaired by chemical grout injection and hydraulic cement. • 4 cleanouts were repaired. • 13 inflow dishes installed. o Smithfield area • 4 manholes were identified for repairs—Repaired by chemical grout injection and hydraulic cement. • Installed 31 inflow dishes. June 2018—Grassy Branch Trunk Sewer • All manholes in the Grassy Branch trunk sewer(outfall)were inspected. o Installed inflow dishes and verified all MH's were sealed and secured from WVVfP to the most upstream point of the system. There were no visible leaks above ground. October 2018—Continuation of I&I efforts in branch sewers in Loxdale subdivision and Grassy Branch Trunk Sewer • Efforts include smoke tests, manhole inspections, and CCTV all services and connections. o No visible detection as a result of test in customer clean-outs. • Inspection of Grassy Branch trunk sewer did not indicate significant issues, only replacing missing bolts in manhole covers. November 2018— I&I efforts from Clontz Long Road to Grassy Branch WVVfP • CCTV survey along Clontz Long Road to Grassy Branch VVVVfP. o A small leak was discovered and repaired at a manhole along the route. • Survey was not completed along entire route. December 2018—Continuation of I&I efforts from Clontz Road to Grassy Branch WVVfP, Loxdale Subdivision, and Smithfield • CCTV crew continued survey along Clontz Road. Efforts stopped due to a large rain event,which prohibited cameras from being deployed. • The Loxdale subdivision survey discovered one leaking sewer lateral that was repaired and one manhole grouted. • CCTV crew conducted mainline survey in Smithfield,ties in to the main trunk line to Grassy Branch WWTP. o No visible detection was reported. 2019— Phase 4 of I&I Efforts • Entire collection system has been surveyed by CCTV. o 42 manholes have been grouted and 48 inflow collectors installed. • Ongoing inspections demonstrated repair work needed in several areas. • County staff continues plug testing during rain events. Page 7/10 APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT III. Additional Flow or Flow Reallocation The County is not able to quantify a specific reduction in influent flow as a result of the on-going l&I reduction efforts. However, the County's l&I reduction efforts have resulted in a slight decrease in the peaking factors at the Grassy Branch VVVVTP. Table III-4 summarizes the annual average, maximum month, maximum 7-day, and maximum day peaking factors (PF)from 2015 through 2018. In 2018, the maximum day peaking factor was 6.72 compared to 7.76 in 2015 prior to l&I reduction efforts. Table III-4: Summary of Historical Influent Peaking Factors Parameter 2015 2016 2017 2018 Maximum month peaking 1.94 1.65 1.74 1.91 factor Maximum week(7-day) 2.98 3.44 2.70 2.72 peaking factor Maximum day peaking 7.76 7.00 6.74 6.72 factor 4. VVVVTP Process Modifications Union County has been actively evaluating process changes at the VVVVTP to minimize NOVs. Staff has taken several precautionary measures in anticipation of high flow events, as follows: • Bypassing of tertiary filters during wet weather events. • Increased monitoring of VVVVTP to include frequent visits during a wet weather event and constant monitoring of telemetry via supervisory control and data acquisition (SCADA). • Control of air input to aeration basins to retain suspended solids: o Shutting down of all compressors except one. o Reducing remaining compressor to 30 Hz. o Shutting down all aerator drop legs except the first set. Additional process changes will not resolve the permit violations. County staff has made all of the feasible process changes and implemented the appropriate operational strategies in an on-going effort to resolve the compliance issues. 5. Additional Flow Request The historical data indicate the influent flows that exceed the permitted design capacity of the Grassy Branch VVVVTP have resulted in final effluent permit violations for flow, conventional pollutants, and bacterial pollutants (refer to Attachment to SOC Application IV. Necessity Narrative). The County has attributed the majority of the NOVs to record rainfall events in the region. However, the County also acknowledges that more sewer connections have been allocated to the Grassy Branch WVVTP than available capacity. APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT Ill. Additional Flow or Flow Reallocation Hazen recommends a permanent increase in the design maximum month flow from 0.05 mgd to 0.120 mgd. The flow increase is associated with the existing domestic flow discharging to the WWTP, the maximum student capacity of the three schools, new connections in the Smithfield subdivision to fulfill contractual obligations, and private parcel connections along the main sewer line to the plant. The Loxdale subdivision has reached the maximum dwelling units for the subdivision. The anticipated planned flow was established using the average day wastewater flow rates published in 15A NCAC 02T .0114 (Wastewater Design Flow Rates). The anticipated planned flow was added to the annual average flow to the WWTP. A maximum month peaking factor of 1.7 was applied to the annual average flow, which results in a maximum month design flow of 0.120 mgd. The peaking factor of 1.7 is the median peaking factor of the 2014 through August 2019 data set. Figure III-3 provides an illustration of the average day and maximum month flows at the WWTP from January 2014 through August 2019 and associated peaking factors. The maximum month peaking factors are significantly higher than what is typical for larger treatment facilities. Table III-5 summarizes the proposed design annual average and maximum month flow. Table III-5: Summary of Methods Used to Calculate Proposed Maximum Month Design Flow Current Anticipated Total Flow, Peaking Dwelling Unit I School Flow, gpd Planned Flow, gpd gpd Factor 9 Piedmont High School ---- 1,953 1,2,3 __-- (1,363 students) Piedmont Middle School ---- 0 4 -- (1,018 students) Unionville Elementary School ---- 0 4 ---- (701 students) Loxdale Subdivision (52 lots) ---- 0 s --- ---- Smithfield Subdivision (70 lots) ---- 1,800 1,6 ---- Private parcels ---- 11,520 ',7 ---- Annual average flow 53,360 15,270 68,630 ---- Maximum month flow 8 ---- ---- 120,000 1.7 Maximum week (7-day) flow ---- ---- 201,000 3.0 Maximum day flow ---- ---- 469,000 7.0 Per 15A NCAC 02T.0114— Wastewater Design Flow Rates. 2 15 gpd/student for average day school flow rate converted to an annual average flow(e.g., school in session 180 days per year). 3 High school is currently 84%enrolled. Maximum capacity is 1,600 students per Union County Public Schools. 4 The middle and elementary schools are at maximum enrollment. 5 The Loxdale subdivision is built out to a maximum of 52 homes. 6 The Smithfield subdivision currently contains five vacant lots. Vacant lots were counted as three bedrooms for planning purposes. Private parcels currently contain 12 dwelling units. Approximately 32 vacant lots are available and were counted as three bedrooms for planning purposes. 8 Rounded to the nearest 10,000 gallons. 9 The maximum month peaking factor is based on the median peaking factor of the January 2014 through August 2019 data set. APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT III. Additional Flow or Flow Reallocation 0.120 — - 3.0 = 2.8 - 2.6 0.100 — - 2.4 - 2.2 0.080 — - 2.0 1.8 o E - 1.6 ti 0.060 — rn _ Qo - 1.4 c • =OPcu - 1.2 a 0.040 — - 1.0 = 0.8 i 0.6 0.020 — : - 0.4 - 0.2 0.000 0.0 2014 2015 2016 2017 2018 2019 mom Maximum Month iim Annual Average —Permit Permit Flow Limit ••4?-• Peaking Factor Figure III-3: Monthly Average, Maximum Month Flow, and Annual Average to Maximum Month Peaking Factors Page 10/10 STATE OF NORTH CAROLINA DEPARTMENT OF ENVIRONMENTAL QUALITY DIVISION OF WATER RESOURES APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT IV. Necessity Narrative 1. Background Union County owns and operates the Grassy Branch WWTP and associated collection system infrastructure. The WWTP is permitted to discharge 0.05 mgd of treated effluent into Crooked Creek via NPDES permit NC0085812. The Grassy Branch WWTP receives only domestic wastewater. Industrial users do not discharge to the WWTP. Additionally, the WWTP does not accept influent wastewater from other municipalities. The WWTP serves three schools, two residential subdivisions, and several private parcels. The County has received Notice of Violations (NOVs) for flow, five-day biochemical oxygen demand (BOD5), ammonia (NH3-N), fecal coliform, total suspended solids (TSS), and pH over the last few years. The Grassy Branch WWTP NOVs are summarized in Table IV-1. The County has attributed the majority of the NOVs to record rainfall events in the region. However, over-allocation of sewer connections to the Grassy Branch WWTP has also contributed to and intensified the compliance issues (refer to Attachment Ill. Additional Flow or Flow Reallocation). Table IV-1: Summary of Notice of Violations for Grassy Branch WWTP Permit Violation Flow BOD5 BOD5 NH3-N NH3-N TSS (monthly (weekly (monthly (weekly (monthly Fecal (weekly Date average) average) average) average) average) Coliform average) pH 1/31/2018 0.058 2/3/2018 23 1,500 2/28/2018 0.07 220 3/3/2018 6,971 3/17/2018 3/31/2018 27.1 3/31/2018 20.3 16.3 6/2/2018 13.2 2,949 10/6/2018 440 10/13/2018 570 10/20/2018 810 10/31/2018 0.056 APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT IV. Necessity Narrative Table IV-1: Summary of Notice of Violations for Grassy Branch WWTP Permit Violation Flow BOD5 BOD5 NH3-N NH3-N TSS (monthly (weekly (monthly (weekly (monthly Fecal (weekly Date average) average) average) average) average) Coliform average) pH 11/10/2018 1,200 11/17/2018 6,000 11/30/2018 0.088 12/11/2018 9.97 12/15/2018 7,200 12/22/2018 16.1 560 12/29/2018 17 6,000 12/31/2018 0.106 4.86 1,448 1/5/2019 737 1/12/2019 23.3 1/31/2019 0.10 2/28/2019 0.07 4/6/2019 193 6,000 177 4/13/2019 14.6 6.05 4/30/2019 0.065 24.8 2.05 2. VWVTP Process Modifications Union County has been actively evaluating process changes at the VVV TP to minimize NOVs. Staff has taken several precautionary measures in anticipation of high flow events, as follows: • Bypassing of tertiary filters during wet weather events. • Increased monitoring of WVVTP to include frequent visits during a wet weather event and constant monitoring of telemetry via supervisory control and data acquisition (SCADA). • Control of air input to aeration basins to retain suspended solids: o Shutting down of all compressors except one. o Reducing remaining compressor to 30 Hz. o Shutting down all aerator drop legs except the first set. Additional process changes will not resolve the permit violations. County staff has made all of the feasible process changes and implemented the appropriate operational strategies in an on-going effort to resolve the compliance issues. APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT IV. Necessity Narrative 3. Collection System Rehabilitation The County has been actively involved in reduction of infiltration and inflow(I&I) in the collection system. A Phase 1 I&I study was commissioned in 2016 to broadly determine problem areas. A Phase 2 study in 2017 focused on repair efforts readily identified in the Phase 1 study. The Phase 2 study also included wet weather monitoring. In 2018, Phase 3 efforts included confirming the effectiveness of previous repair efforts, extensive CCTV review of the entire collection system, and the continuation of repair efforts. Phase 4 of the l&I reduction effort was initiated in January 2019. This phase consists of a review of dry and wet weather data and patterns and on-going inspection of the collection system. As of January 2019, the entire Grassy Branch collection system has been surveyed by closed-circuit television (CCTV). As of May 2019, 42 manholes have been grouted and 48 inflow collectors installed. Table IV-2 provides a summary of the maintenance data for the I&I reduction effort from 2014 to present, including investigative man hours and quantity of repaired infrastructure (e.g., manholes, laterals, etc.). A detailed summary and timeline of the County's l&I reduction efforts is located in Attachment III (Additional Flow or Flow Reallocation). Table IV-2: Summary of ICI Effort Maintenance Data 2014 2015 2016 2017 2018 2019 Man Hours Investigating 960 1080 960 480 1512 1152 Man Hours Repairing 360 48 0 72 1152 192 Footage Cleaned 0 0 10,181 425 10,146 CCTV Footage 160 40 10,181 160 16,273 14,627 Hours Smoke Testing 24 20 36 36 37 32 Smoke Test Footage 14,745 7,283 4,235 4,570 15,308 8,368 Manholes Repaired 3 0 0 0 42 3 Lateral Repaired 6 4 0 4 25 8 Cleanouts Repaired 6 4 0 4 17 8 Inflow Dishes Installed 0 0 0 0 53 0 APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT IV. Necessity Narrative 4. Unavoidable Future Violations Figures IV-1 through IV-4 compare the final effluent monthly average BOD5, TSS, ammonia, and fecal coliform concentrations to the WWTP permitted capacity, respectively. The effluent BOD5 exceedances have typically occurred during the cold weather months of the year since 2015. Effluent TSS was exceeded in 2015 and again in April 2019. Weekly and monthly averages for ammonia have been exceeded, particularly in the colder months. Fecal coliform violations have occurred since 2015 regardless of season. The historical data indicate influent flows greater than the permitted maximum month design flow results in final effluent permit violations for flow, BOD5, ammonia, and fecal coliform. Per the evaluation provided in Attachment III (Additional Flow or Flow Reallocation), the majority of the NOVs are attributed to record rainfall events in the region. However, it is acknowledged that over-allocation of sewer connections to the Grassy Branch WWTP has contributed to and intensified the compliance issues. The County's continued I&I rehabilitation efforts have resulted in a slight reduction in the peaking factors; however, the average day flow to the WWTP has not significantly decreased. The existing Grassy Branch WWTP treatment infrastructure will not support compliance with the current effluent permit limits. The violations will continue to occur without infrastructure improvements. The WWTP must not receive an NOV during the consent order timeframe. The proposed interim monthly average effluent limits are provided in Table IV-3. The proposed interim effluent limits do not include a weekly average limit. It is anticipated that during construction, a weekly average limit will be difficult to meet and will likely result in NOVs. The proposed interim limits were developed based on the current performance of the WWTP prior to the upgrade and improvements to existing infrastructure. Interim limits are proposed for BOD5, TSS, ammonia, and fecal coliform. Changes are not being proposed for the current effluent permit limit for dissolved oxygen at 5 mg/L. The justification for the effluent limits for each pollutant are as follows: • BOD5—With exception of one data point in March 2015, the WWTP has consistently achieved a monthly average BOD limit of 30 mg/L in winter and summer months. The process evaluation confirmed the reliability of the existing secondary treatment process to meet the proposed monthly average BOD limit of 30 mg/L in winter and summer. The secondary process is not equipped with the volume or aeration capacity to reliably meet less than 30 mg/L BOD without raising the risk of a NOV. • TSS—A monthly average of 100 mg/L is proposed as an interim effluent limit. With the exception of a March 2019 data point, the WWTP has consistently achieved less than 60 mg/L of effluent TSS. However, the calculated hydraulic and solids loading rates to the existing filters are excessive compared to standard engineering practice. Therefore, the proposed interim effluent TSS limit of 100 mg/L was established to avoid future NOVs as a result of limited solids handling and filter capacity at the WWTP. • Ammonia—A monthly average of 20 mg/L and 6 mg/L ammonia is proposed as interim -- effluent limits in the winter and summer months, respectively. The historical data indicates that the WWTP has consistently achieved 20 mg/L in the winter and 6 mg/L in APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT IV. Necessity Narrative the summer. The secondary process is not equipped with the volume or aeration capacity to reliably meet less than the proposed summer and winter interim limits without increasing the risk of an NOV during the SOC timeframe. • Fecal coliform—A monthly average limit of 900/100 mL is proposed as in interim effluent limit for fecal coliform. The existing UV system cannot be further optimized and does not have the required capacity to meet the proposed maximum month design flow of 0.12 mgd. The highest monthly geometric mean occurred in December 2018 with a result of approximately 758/100 mL. The capacity of the existing UV system is not sufficient to meet a weekly average limit or a daily maximum during the SOC timeframe. • Dissolved oxygen — No changes are proposed for the effluent dissolved oxygen limit of greater than 5 mg/L. Table IV-3: Proposed Interim Effluent Limits Monthly Average Weekly Average Interim flow, mgd 0.120 BOD5, mg/L(November 1 through March 31) 30 BOD5, mg/L(April 1 through October 31) 30 TSS, mg/L 100 Ammonia, mg/L(November 1 through March 31) 20 Ammonia, mg/L(April 1 through October 31) 6 Fecal coliform, geometric mean/100 mL 900 Dissolved oxygen, mg/L >5 The QUAL2K modeling results (Tetra Tech, 2019) support the proposed interim effluent limits. The calibrated baseline wasteload model demonstrated strong performance results and captured key dissolved oxygen trends in Crooked Creek. The calibrated QUAL2K model was then used to assess the impact of the Grassy Branch V V TP expansion flow for both the interim and final proposed effluent limits. The model demonstrates that there is assimilative capacity for both the interim SOC and final effluent permit limits. The instream dissolved oxygen standard of 5 mg/L was met in all conditions. The model results also demonstrated that ammonia toxicity will not be exceeded. APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT IV. Necessity Narrative 40 • 35 30 • • 25 • rn • • 0 20 b • U •♦ • o15 ----1 ♦ 1 1 r---t- U 4 ♦ 10 $ �!♦� I ♦ A ♦ ♦ • �! ♦ ♦ t ♦ • • • r ♦ ♦% ♦ ♦ ► ♦ i�► AAA A 41111AAA • %A AllrartsmitridA4A aimill•• • • Aiminia 0 ♦ ♦ ♦ ♦ Jan-15 Jul-15 Jan-16 Jul-16 Jan-17 Jul-17 Jan-18 Jul-18 Jan-19 Jul-19 Jan-20 ----Weekly Average Permit Limit Monthly Average Permit Limit ♦ Weekly Average Effluent BOD • Monthly Average Effluent BOD Figure IV-1: Grassy Branch WWTP Effluent BOD with respect to Permit Limit facie 6/9 APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT IV. Necessity Narrative 200 180 ♦ 160 140 120 rn E 0 100 a) 80 0 c 0 U 60 • • A.40 ♦ ♦ • 20 • • • ♦ •♦• ♦ ♦ • Jan-15 Jul-15 Jan-16 Jul-16 Jan-17 Jul-17 Jan-18 Jul-18 Jan-19 Jul-19 Jan-20 ----Weekly Permit Limit Monthly Permit Limit A Weekly Average Effluent TSS • Monthly Average Effluent TSS Figure IV-2: Grassy Branch WWTP Effluent TSS with respect to Permit Limit Page 7/9 APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT IV. Necessity Narrative 30 25 • • 20 J O) C ♦ 0 t 15 L c a) c ---- ♦ f 0 10 • ♦ ♦• ♦ 5 �� ♦ • ♦ 6 ♦ • • • oi ♦ ♦ • ♦�,► tA Au&sitii• r♦ ♦ i • ♦ ♦ 0 Jan-15 Jul-15 Jan-16 Jul-16 Jan-17 Jul-17 Jan-18 Jul-18 Jan-19 Jul-19 Jan-20 ----Weekly Permit Limit Monthly Permit Limit ♦ Weekly Average Effluent Ammonia • Monthly Average Effluent Ammonia Figure IV-3: Grassy Branch WWTP Effluent Ammonia with respect to Permit Limit Page 8/9 APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT IV. Necessity Narrative 100,000 • 10,000 ♦ ♦ ♦♦♦ • • • • - 1,000 • o ♦ � 0 ♦ •♦ l A L • A • •♦ ♦ ♦ ♦ ♦a A .11' U ♦ ♦♦ ♦ ♦+ ♦ ♦ • ♦ 00 100 ♦• ♦ • ♦ ♦ A •♦ ♦ ♦♦ ♦♦ • :♦ ♦♦• ♦ ••♦ ♦� ♦A ♦♦ • A c ' •Il► ♦y ♦a ♦ � ♦♦ •♦ ♦ o ♦ lA4♦ 4 • ♦ i ♦ ♦ ♦ ♦ • ♦ A. 10 • • • • • • ♦ ♦ ' ♦% ♦ �♦ ♦ ♦ • • •♦• AA ' • • •• ♦ ♦ • • • ♦ • 4 • ♦ • ♦ ♦♦, •• •♦ •'♦ • ♦ 1♦ ♦ • ♦i ♦ • ♦ ♦ ♦' A ♦ ♦ ♦ ♦ ♦ ' ♦ ♦ • •• ♦' •• •1► ♦ ♦ ♦ ♦• • ♦ •Y ♦ ♦ ♦ 1 41 W ♦ Y ♦ YAM ♦♦ /A ♦ Y♦♦ ♦ ♦ d&♦ Jan-15 Jul-15 Jan-16 Jul-16 Jan-17 Jul-17 Jan-18 Jul-18 Jan-19 Jul-19 Jan-20 ----Weekly Permit Limit Monthly Permit Limit ♦ Weekly Average Effluent Fecal Coliform • Monthly Average Effluent Fecal Coliform Figure IV-4: Grassy Branch WWTP Effluent Fecal Coliform with respect to Permit Limit Page 9/9 I I STATE OF NORTH CAROLINA DEPARTMENT OF ENVIRONMENTAL QUALITY DIVISION OF WATER RESOURES APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT V. Engineer Certification Hazen Technical Memorandum North Carolina License C-0381 December 3,2019tN�� * To: Union County Department of Public Works ' A IfiIP From: Jim Struve, PE, Hazen and Sawyer(Hazen) )8179 Mary Sadler, PE, Hazen toils Joe Rohrbacher, PE, Hazen Michael Parker, PE, Hazen N Amanda Ford, Hazen Engineer Certification for Grassy Branch Wastewater Treatment Plant Special Order by Consent 1. Introduction This process certification is in support of the Union County Public Works(UCPW)application for a Special Order by Consent(SOC)for the Grassy Branch Wastewater Treatment Plant(WWTP). This correspondence is an independent professional report on the status of the Grassy Branch WWTP to meet the existing National Pollutant Discharge Elimination System (NPDES)permit limits during the period the WWTP will be operating under the SOC. The following narratives specifically address the SOC application requirements. It should be noted that all engineering determinations are supported by a detailed process evaluation published separately from this signed and sealed certification. 2. Summary of Existing WWTP Infrastructure The Grassy Branch WWTP is an extended aeration package treatment plant(PTP)constructed by Hydro- Aerobics Package Wastewater Treatment Systems in 1997. The WWTP is permitted for a maximum month design flow of 50,000 gallons per day(gpd), or 0.05 million gallons per day(mgd)to the Crooked Creek receiving stream,a Class C water. Union County operates the facility NPDES permit NC0085812. Table 2-1 summarizes the current final effluent permit limits for five-day biochemical oxygen demand (BOD5),total suspended solids(TSS), ammonia(NH3-N), and fecal coliform. The Grassy Branch WWTP consists of coarse screening, flow equalization,two conventional aeration basins with coarse bubble diffusers,two secondary clarifiers,a sand filter,and ultraviolet(UV) disinfection. Waste activated sludge(WAS)is processed in an aerobic digester for volatile solids reduction. The digested solids are then pumped to a tanker truck and transported to the Crooked Creek WWTP for further stabilization. Table 2-2 summarizes the design criteria of the existing Grassy Branch WWTP infrastructure. Hazen and Sawyer•9101 Southern Pine Blvd. Suite 250•Charlotte. NC 28273 •704 357 3150 Hazen Table 2-1: Current Final Effluent Permit Limits Monthly Weekly Parameter Average Average BOD5, mg/L(April 1 through October 31) 5 7.5 BOD5, mg/L(November 1 through March 31) 10 15 TSS, mg/L 30 45 Ammonia, mg/L(April 1 through October 31) 2 6 Ammonia, mg/L (November 1 through March 31) 4 12 Fecal coliform, geometric mean/100 mL 200 400 Dissolved oxygen, mg/L >5 Table 2-2: Summary of Design Criteria for Existing Grassy Branch WWTP Infrastructure Unit Process Parameter Design Criteria Number of pumps 2 Capacity Influent PumpStation p yper pump, gpd 129,600 Capacity total, gpd 259,200 Type Coarse Manual Bar Screen Influent Screening Number 1 Opening diameter, inch 2 Number 2 Volume per basin,gallon 7,700 Flow Equalization Volume total, gallon 15,400 Type of aeration system Coarse bubble Number of blowers 2 Flow Equalization Type of blowers Positive displacement Treatment Aeration System Motor, horsepower(HP) 2 Number 2 Secondary Treatment Volume per basin,gallon 25,000 Engineer Certification for Grasse Branch \\asto+ater Treatment Plant Page 2 of I I Hazen Table 2-2: Summary of Design Criteria for Existing Grassy Branch WWTP Infrastructure Unit Process Parameter Design Criteria Volume total, gallon 50,000 Hydraulic retention time per basin, hour 12 Hydraulic retention time total, hour 24 Type of aeration system Coarse bubble Secondary Treatment Number of blowers 2 Aeration System Type of blowers Positive displacement Motor, horsepower(HP) 7.5 Number of clarifiers 2 Secondary Clarifier Diameter,feet 10 Surface area, SF 78.5 Number of beds 2 Area of bed per unit, SF 18.75 Sand Filter Area of bed total, SF 37.5 Fill material Anthracite/Sand Number of blowers 2 Sand Filter Aeration Type of blowers Positive displacement System Motor, horsepower(HP) 3 Number of banks 2 Ultraviolet Disinfection Number of modules 3 Number of lamps per module 2 3. Flow Evaluation The historical data indicate that influent flows in excess of the permitted design capacity of the WWTP have resulted in final effluent permit violations for flow, conventional pollutants, and bacterial pollutants. The County has attributed the majority of the Notice of Violations(NOVs)to record rainfall events in the region. The County also acknowledges that more sewer connections have been allocated to the Grassy Branch WWTP than available capacity. L,neineer Certification for Grassy Branch wastewater Treatment Plant Hazen Hazen recommends a permanent increase in the design maximum month flow from 0.05 mgd to 0.120 mgd. The flow increase is associated with the existing domestic flow discharging to the WWTP,the maximum student capacity of the three schools, new connections in the Smithfield subdivision to fulfill contractual obligations, and private parcel connections along the main sewer line to the plant. The Loxdale subdivision has reached the maximum dwelling units for the subdivision. The anticipated planned flow was established using the average day wastewater flow rates published in 15A NCAC 02T .0114 (Wastewater Design Flow Rates). The anticipated planned flow was added to the annual average flow to the WWTP. A maximum month peaking factor of 1.7 was applied to the annual average flow, which results in a maximum month design flow of 0.120 mgd. The peaking factor of 1.7 is the median peaking factor of the 2014 through August 2019 data set. The maximum month peaking factors at the Grassy Branch WWTP are significantly higher than what is typical for larger treatment facilities. Table 3-4 summarizes the proposed design annual average and maximum month flow. Table 3-4: Summary of Methods Used to Calculate Proposed Maximum Month Design Flow Current Anticipated Total Flow, Peaking Dwelling Unit/School Flow, gpd Planned Flow, gpd gpd Factor 9 Piedmont High School 1,953 ' 2 ; (1,363 students) Piedmont Middle School ---- 0 4 (1,018 students) Unionville Elementary School ---- 0 4 (701 students) Loxdale Subdivision (52 lots) ---- 0 5 Smithfield Subdivision (70 lots) ---- 1,800' 6 Private parcels ---- 11,520'.7 Annual average flow 53,360 15,270 68,630 Maximum month flow 8 ---- ---- 120,000 1.7 Maximum week (7-day)flow ---- ---- 201,000 3.0 Maximum day flow ---- ---- 469,000 7.0 'Per 15A NCAC 02T.0114—Wastewater Design Flow Rates. 2 15 gpd/student for average day school flow rate converted to an annual average flow(e.g., school in session 180 days per year). 3 High school is currently 84%enrolled. Maximum capacity is 1,600 students per Union County Public Schools. 4 The middle and elementary schools are at maximum enrollment. 5 The Loxdale subdivision is built out to a maximum of 52 homes. 6 The Smithfield subdivision currently contains five vacant lots. Vacant lots were counted as three bedrooms for planning purposes. Private parcels currently contain 12 dwelling units. Approximately 32 vacant lots are available and were counted as three bedrooms for planning purposes. 8 Rounded to the nearest 10,000 gallons. 9 The maximum month peaking factor is based on the median peaking factor of the January 2014 through August 2019 data set. Engineer Certification for Grasse Branch Wasto‘ater"Treatment Plant I'.i-J 01 11 Hazen 4. Evaluation and Optimization of Existing Treatment Units 4.1 Historical Influent Characterization Data Tables 4-1 and 4-2 summarize the maximum month, maximum week(e.g., 7-day), and maximum day peaking factors(PF)and influent concentrations and loads, respectively. Data was evaluated from 2015 through 2018. Data from the year 2019 does not account for the impact of the seasonal flow variation and was therefore not included in the analysis. A statistical approach was used for evaluating influent characterization metrics and peaking factors. The original design influent loads and concentrations for the WWTP are not known, as the criteria were not provided in the manufacturer's Wastewater Treatment Systems Operations and Maintenance(O&M) manual. The proposed design concentrations and loads for the Grassy Branch WWTP improvements project are summarized in Table 4-3. Table 4-1: Influent Flow and Peaking Factors Parameter 2015 2016 2017 2018 Maximum month peaking factor 1.94 1.65 1.74 1.91 Maximum week (7-day) peaking factor 2.98 3.44 2.70 2.72 Maximum day peaking factor 7.76 7.00 6.74 6.72 Table 4-2: Annual Average Influent Concentrations and Loads Parameter 2015 2016 2017 2018 BOD5, mg/L 135 185 217 203 BOD5, Ib/d 46 59 69 87 TSS, mg/L 184 325 462 458 TSS, Ib/d 63 98 137 170 NH3-N, mg/L 33 33 27 29 NH3-N, Ib/d 10 11 9 11 Engineer Certification for Grasse Branch WastoNater I reatment Plant Page 5 of II Hazen Table 4-3: Proposed Influent Design Concentrations and Loads Concentration, Maximum Month Maximum Week Maximum Day Parameter mgIL Load, Ib/d Peaking Factor Peaking Factor Peaking Factor TSS 250 140 1.2 1.5 2.0 BOD5 250 140 1.2 1.5 2.0 TKN 40 22 1.2 1.5 2.0 N H 3-N 26 15 1.2 1.5 2.0 Total 5.0 2.8 1.2 1.5 2.0 phosphorus 4.2 Influent Pumps The existing influent pumps are rated at 130,000 gpd each at 15 feet of total dynamic head(TDH),which allows for 260,000 gpd with both units in service. The existing pumps cannot be further optimized and do not have sufficient capacity for the proposed maximum month design flow. Additional pumps will be needed to provide adequate capacity with redundancy for the proposed improvements. 4.3 Influent Screening Influent screening is comprised of a manual coarse bar screen designed for a peak hour flow of 150,000 gpd(e.g.,2.5 times the maximum month design flow of 50,000 gpd). The existing bar screen cannot be further optimized. Additional screening unit(s)are required as the existing screen does not have adequate capacity to meet the proposed maximum month design flow. 4.4 Flow Equalization Existing flow equalization consists of two 7,700-gallon basins,or 15,400 gallons total volume. The existing flow equalization basins cannot be further optimized, as the basins do not provide adequate hydraulic retention time to attenuate the proposed maximum month design flow.Additional equalization volume is required as part of the facility improvements. 4.5 Secondary Treatment Train The secondary treatment process consists of a 50,000 gpd(e.g.,two trains in service)conventional aeration activated sludge process. The PTP is equipped with coarse bubble diffusers and two rotary lobe positive displacement blowers. The aeration basins were designed to provide a 24-hour hydraulic retention time at the current maximum month design flow of 0.05 mgd. However, only 15 hours of hydraulic retention time is provided at current flows. The WAS flow is not measured nor were solids hauling records available for the determination of the solids retention time(SRT). The positive displacement blowers and coarse bubble aeration system does not have adequate capacity to treat the 1 ncinecr Certification for Grass Branch Wastes+ater I rcatment Plant Page 6 of 1 1 Hazen existing annual average,maximum month,maximum week, and maximum day loads with one blower out of service. Based on the available hydraulic,process, and equipment capacity,the secondary process cannot be further optimized to treat additional flow.New process volume and aeration equipment is required as part of the facility improvements for the proposed maximum month design flow. 4.6 Secondary Clarifiers The Grassy Branch WWTP has two 10 foot diameter secondary clarifiers.Each clarifier has a sidewater depth of 10 feet. The reported historical peak day surface overflow rates(SOR)and surface loading rates (SLR)are 1,823 gpd/SF and 63 lb/SF,respectively. The calculated overflow and loading rates are excessive compared to standard engineering best practices. Typical design overflow rates range from 300 to 1,000 gpd/SF. Typical solids loading rates range from 15 to 35 lb/day-SF. The existing secondary clarifiers are undersized and cannot be further optimized.New secondary clarification capacity is required for the proposed improvements. 4.7 Tertiary Filtration The WWTP has two mixed media(anthracite/sand)tertiary filters each with a surface area of 18.75 SF. The historic peak day hydraulic loading rate and solids loading rate are 7.3 gpm/SF and 3.9 lb/SF, respectively. The calculated hydraulic and solids loading rates are excessive compared to standard engineering best practices.Typical filter design hydraulic and solids loading rates are 5 gpd/SF and 3 lb/day-SF,respectively. The existing mixed media filters cannot be further optimized.New filtration capacity is required for the proposed improvements. 4.8 UV Disinfection The existing UV disinfection system was installed in the original chlorine contact chamber as a retrofit project. Routine maintenance is problematic as it requires that UCPW staff remove grating and stand in the channel. The existing UV system cannot be further optimized and does not have the required capacity to meet the proposed maximum month design flow. An additional unit(s)will be required to meet the proposed peak day flow. 4.9 Effluent Flow Measurement Effluent flow is measured via a discharge weir. The existing weir will require replacement to accommodate the proposed maximum month design flow. 4.10 Post Aeration The facility does not have a formal post aeration system. Aeration is achieved through the effluent flow weir and head drop to the final effluent discharge location. The facility has not had any effluent permit violations for dissolved oxygen, so it is not anticipated that additional post aeration capacity will be needed. Engineer Certification for Grasse Branch ti astex\ater"treatment Plant Page 7 of I I Hazen 4.11 Aerobic Digester The existing aerobic digester equalization consists of two 4,500-gallon basins for 9,000 gallons of total volume. The aerobic digester is equipped with coarse bubble diffusers connected to the secondary treatment positive displacement blowers. The aerobically digested solids are pumped out and transported to the Crooked Creek WWTP for final disposal.Additional aerobic digestion volume will be needed to accommodate the proposed maximum design flow. The final disposal method will not be altered. 4.12 Operational Procedures Current operating procedures are consistent with best practices for operation of a wastewater treatment facility. Housekeeping and maintenance of the facility are excellent for industry standards.No operational changes are recommended at this time. 5. Specific Requirements of the SOC 5.1 Evaluation of Existing Treatment Units and Operational Procedures The existing Grassy Branch WWTP does not have adequate process capacity to adequately treat the current flows and loads and maintain NPDES permit compliance. The WWTP cannot be further optimized or operated in a manner that achieves compliance with final effluent permit limits. Additional process units are necessary for compliance with the existing final effluent permit limits. 5.2 Effluent Limits that the Facility Could Be Expected to Meet if Operated at Maximum Efficiency during the Term of the Requested SOC (Consider Interim Construction Phases) The historical data indicate that influent flows greater than the permitted maximum month design flow will result in final effluent permit violations for flow,BOD5, TSS, ammonia, and fecal coliform. Table 5-1 summarizes the requested interim effluent limits for the Grassy Branch WWTP. The requested limits are based on the 2015 to August 2019 historical data in conjunction with the process modeling and WWTP evaluation. It is not anticipated that construction phases will be applicable to the proposed upgrade project, so tiered interim limits are not provided. 5.3 Effluent Limits after Expansion and Upgrade of WWTP Speculative limits were informally discussed with the Division of Water Resources(DWR)for the upgraded and expanded Grassy Branch WWTP during the process of preparing the SOC application package. DWR responded that a receiving stream model was necessary to assess water quality impacts of the expanded flow. The County conducted a site-specific QUAL2K model of the Crooked Creek receiving stream in 2016 and 2017 as part of a broader master planning process. A Final Study Plan was approved by DWR in July 2016. Site-specific sampling was conducted in August 2016. A draft model report was submitted to the County in 2017. F;ngincer Certification for Grassy Branch astc\\atcr"treatment Plant Page 8 of 11 Hazen Table 5-1: Interim Effluent Permit Limits Request Parameter Monthly Average Weekly Average Interim flow, mgd 0.120 BOD5, mg/L(November 1 through March 31) 30 BOD5, mg/L(April 1 through October 31) 30 TSS, mg/L 100 Ammonia, mg/L(November 1 through March 31) 20 Ammonia, mg/L(April 1 through October 31) 6 Fecal coliform,geometric mean/100 mL 900 Dissolved oxygen, mg/L > 5 The QUAL2K model was updated in late summer 2019 to serve as a baseline wasteload model of existing conditions in the Crooked Creek receiving stream. The model was submitted to DWR staff for review in August 2019. A meeting was held with DWR staff on October 1, 2019 to discuss the model calibration, verification,and performance results.Attachment A of this Engineering Certification provides the Crooked Creek QUAL2K Model Development Report(Tetra Tech,October 2019). The model demonstrated strong performance results and captured key dissolved oxygen trends. Interim and final permit limits were also discussed during the meeting with DWR on October 1,2019. Per 15A NCAC 02B .0206(d)(1), if the 7Q10 receiving stream flow is estimated to be zero and if the 30Q2 flows are estimated to be greater than zero,the minimum flow requirements are a BOD concentration of 5 mg/L, an ammonia concentration of 2 mg/L,and a dissolved oxygen concentration of 6 mg/L. A 1 mg/L ammonia threshold is typically applied to address ammonia toxicity. Based on the discussion during the October 1,2019 meeting with DWR staff,Table 5-2 provides a summary of the anticipated effluent limits for the upgraded and expanded WWTP. A major NPDES permit modification and an engineering alternatives analysis will be required for the permanent flow increase. The calibrated QUAL2K model was then used to assess the impact of the Grassy Branch WWTP expansion flow for both the interim and final proposed effluent limits. The Crooked Creek Model Application Report for the Grassy Branch WWTP(Tetra Tech, October 2019) is located in Attachment B. The model demonstrates that there is assimilative capacity for both the interim SOC and final effluent permit limits. The instream dissolved oxygen standard of 5 mg/L was met in all conditions. The model results also demonstrated that ammonia toxicity will not be exceeded. One of the issues raised by DWR staff during the October 1,2019 meeting was the impact of the Grassy Branch WWTP expansion on downstream turbidity impairment in the Rocky River. Significant sources of turbidity in the Rocky River watershed have been associated with stormwater run-off and sediment erosion during rain events.The steady state QUAL2K model does simulate output for TSS. Tetra Tech conducted a statistical analysis of the relationship between TSS and turbidity at four downstream ambient Engineer Certification for Grasse Branch N astowater'lreatment Plant Page 9 of 11 Hazen water quality sampling sites. Tetra Tech concluded that an expansion of the Grassy Branch WWTP is unlikely to contribute to the downstream turbidity impairment. The impact of the Grassy Branch WWTP low effluent flow compared to turbidity contribution from precipitation events is negligible. Table 5-2: Anticipated Final Effluent Permit Limits for the Upgraded and Expanded WWTP Parameter Monthly Average Weekly Average Flow, mgd 0.120 BOD5, mg/L(April 1 through October 31) 5 7.5 BOD5, mg/L(November 1 through March 31) 10 15 TSS, mg/L 30 45 Ammonia, mg/L(April 1 through October 31) 1 2 Ammonia,mg/L(November 1 through March 31) 2 6 Fecal coliform, geometric mean/100 mL 200 400 Dissolved oxygen, mg/L >6 5.4 Any Other Actions Taken to Correct Problems Prior to Requesting the SOC The County has been actively involved in reduction of infiltration and inflow(I&I) in the collection system. A Phase 1 I&I study was commissioned in 2016 to broadly determine problem areas.A Phase 2 study in 2017 focused on repair efforts readily identified in the Phase 1 study. The Phase 2 study also included wet weather monitoring. In 2018, Phase 3 efforts included confirming the effectiveness of previous repair efforts, extensive closed-circuit television (CCTV)review of the entire collection system, and the continuation of repair efforts. Phase 4 of the 1&I reduction effort started in 2019. This phase consists of a review of dry and wet weather data and patterns and on-going inspection of the collection system.As of January 2019,the entire Grassy collection system has been surveyed by CCTV. As of May 2019,42 manholes have been grouted and 48 inflow collectors installed. County anticipates continuing I&I efforts in the Grassy Branch WWTP collection system. Union County has also been actively evaluating process changes at the WWTP to minimize NOVs. Staff has taken several precautionary measures in anticipation of high flow events,as follows: • Bypassing of filters. • Increased monitoring of WWTP to include frequent visits during a wet weather event and constant monitoring of telemetry via SCADA. • Control of air input to aeration basins to retain suspended solids: o Shutting down of all compressors except one. • Engineer Certification for Gras* Branch 14 astowater Treatment Plant Page 10 of 1 Hazen o Reducing remaining compressor to 30 Hz. o Shutting down all aerator drop legs except the first set. 6. Summary of Recommendations for Infrastructure Improvements The historical data indicate the influent flows that exceed the permitted design capacity of the Grassy Branch WWTP have resulted in final effluent permit violations for flow,conventional pollutants, and bacterial pollutants. The County has attributed the majority of the NOVs to record rainfall events in the region. The County also acknowledges that more sewer connections have been allocated to the Grassy Branch WWTP than available capacity. Hazen recommends a permanent increase in the design maximum month flow from 0.05 mgd to 0.120 mgd. Hazen recommends an expansion of the Grassy Branch WWTP to include the following improvements: • Larger influent pumps. • A retrofit of the existing aeration basin coarse bubble diffusers to fine bubble diffuser equipment. • One additional package secondary treatment train to include volume for flow equalization. • New positive displacement blowers serving the existing and new aeration basins. • An additional secondary clarifier. • A new cloth disk filter. • A new UV disinfection system. • Additional volume for aerobic digestion. It is not anticipated that post aeration equipment will be needed for the plant expansion based on the current plant performance. Plant hydraulics would be evaluated during detail design. Existing unit processes will remain in service during construction. It is not anticipated that construction activity will affect the current facility performance. Engineer Certification for Grasse Branch WasteNcater Treatment Plant Page I I of I I Hazen Attachment A: Crooked Creek QUAL2K Model Development, Tetra Tech, October 15, 2019 Crooked Creek QUAL2K Model Development Union County, North Carolina October 15, 2019 PREPARED FOR PREPARED BY Union County Public Works Tetra Tech 500 North Main Street, Suite 500 One Park Drive, Suite 200 Monroe, NC 28112 PO Box 14409 Research Triangle Park, NC 27709 • .. try } " 4,1 117 • _ - • Pictured.'North Fork Crooked Creek(Tetra Tech, 2016) TETRA TECH (This page was intentionally left blank.) Crooked Creek QUAL2K Model October 15, 2019 EXECUTIVE SUMMARY The Crooked Creek watershed in Union County, North Carolina supports three existing wastewater treatment plants (WWTPs): Hemby Acres, Crooked Creek#2, and Grassy Branch. These VWVTPs discharge treated effluent directly into Crooked Creek. There are a number of tributaries across the watershed including the North Fork and South Fork of Crooked Creek, and Grassy Branch which is the most downstream before the confluence with the Rocky River (Figure 1). 1 Rocky County ly J Crooked Creek Grassy Branch VVWTP South Carolina { NorthFork I Crooked Creek i 1 Hemby Acres AIWWT �, / Crooked Creek#2 ir . 1 ® T r. ' , ig, Grassy Branch 4 11014.• 41110,;•• 11. 4A , .. ii,,,,,. ,,„... ,,,1„,4„, ` South Fork Le end Crooked Creek 9 . , A Existing WWTP Outfall River/Stream Highway Crooked Creek Watershed N o o s 1 2 _ Watershed Boundary fit]TETRA TECH WWTP Outfalls ^ ... Kilometers 0 o s z County Boundary NAL'963 suwv.«.a HnV_G.rww0vs.v00,•.0 OM,Ies Map p3.CM 00.07.20tp.H Yen. Figure 1. Crooked Creek watershed map A QUAL2K river water quality model was developed to evaluate the existing conditions along Crooked Creek. The baseline model of existing conditions along Crooked Creek was built, calibrated, and corroborated using monitoring data collected during the summer of 2016. Monitoring results and other criteria were used to break the modeled receiving stream into six model stream reaches (Figure 2). {It)TETRA TECH ES-1 Crooked Creek QUAL2K Model October 15, 2019 Rocky River / 6n / of Grassy Branch WWTP . w ( ilitillik \ Thf Crooked Creel'HembyAcresWWTP ".. ,. 4441 Crooked Creek WWTP ill2• c`r r ir „ - i o = Gce North Fork Crooked Creek ..» ' ete� Legend n.e Ge A WWTP Discharge aver rho RvereStream Dam �Vl QWatershed Boundary Model Reach 1 --e. Reach t Reach I Reach 3 Reach a 1 Crooked Creek Watershed N 0 0 5 1 2 .� Reach 6 [it) TETRA TECH QUAL2K Model Segmentation ^ OKrlometers , Reach 6 N\ v+. no.c,.-.r.dm c aw_rios_uco_v.M OMIles 6W W ea r,.06.01.I01e.M eeece Figure 2. Crooked Creek QUAL2K model reach segmentation A strong model calibration result was achieved for DO (Figure 3). The model simulation of daily average DO concentration captured key trends along the stream longitudinally, particularly in accounting for diurnal variation. A model corroboration simulation also demonstrated a similarly strong model performance (Figure 4). Sensitivity analyses revealed that the model was most sensitive to assumptions for sediment oxygen demand and reaeration, but results were relatively robust given strong assumptions based on good monitoring data. lirt)TETRA TECH ES_2 Crooked Creek QUAL2K Model October 15, 2019 I--1--I------2------I------3---- I---4 I----- 5-- I 6 — ----____ -I i Hemby CC#2 • SFCC HWY Grassy WWTP, WWTP WWTP confluence 601 Grassy Branch confluence I I IBeaver 10 Dams I ____ ' 8 • E _ ------ - �'-• 0 •• :. •• �,' VD 1 ' 1 • • 6 X I • •1 • dJ i Y..Ohl . 1 • , O�• • a•• � • • o L ` X. :• O , •• 2 `..O 0 20 15 10 5 0 Distance from outlet(miles) • YPDRBA Point Data 0 Obs Long Data(AM)Trip 1 • Obg Long Data(PM)Trip 1 o Obs Long Data(AM)Trip 2 • Obs Long Data(PM)Trip 2 Simulated Mean ---- Simulated Min/Max Observed Sonde Data --WQS:5.0 mg/I DO Saturation Figure 3. Simulated and observed DO along Crooked Creek (calibration) I--1--I 2 I 3 I 4-----I 5 I — — 6 --I 1 z Hemby CC#2 SFCC HWY Grassy WWTP, WWTP WWTP confluence 601 Grassy Branch confluence Beaver I I I Dams I 10 j(--'1—f -------- + S. `` - - - 1 i• • • 8 � E I • 1 I O • c I 1 , jiD O • m i V , Os 1 • • 1 O 1 2 0 20 15 10 5 0 Distance from outlet(miles) • YPDRBA Point Data 0 Obs Long Data(AM) • Obs Long Data(PM) Simulated Mean ---- Simulated Min/Max Observed Sonde Data WQS:5.0 mg/I DO Saturation Figure 4. Simulated and observed DO along Crooked Creek (corroboration) fit]TETRA TECH ES-3 Crooked Creek QUAL2K Model October 15, 2019 TABLE OF CONTENTS 1.0 INTRODUCTION 1 2.0 SUMMARY OF AVAILABLE DATA 3 2.1 Goose and Crooked Creeks LWP 3 2.2 Permitted Point Source Monitoring 3 2.3 YPDRBA(Coalition) Instream Sampling 5 2.4 Tetra Tech Sampling 5 2.5 HEC-RAS Modeling Efforts 6 2.6 Goose and Crooked Creek LSPC Model 6 3.0 QUAL2K MODEL SETUP 8 3.1 Model Documentation 8 3.2 Model Date Selection 8 3.3 Model Segmentation 8 3.4 Reach Hydraulics 10 3.5 Meteorological Inputs, Light and Heat 12 3.5.1 Hourly Inputs 12 3.5.2 Light and Heat Inputs 14 3.6 Carbonaceous Biochemical Oxygen Demand Simulation 15 3.7 Boundary Conditions 15 3.7.1 Headwaters 15 3.7.2 Point Source Flows and Water Quality 19 3.7.3 Tributary Flows and Water Quality 22 3.8 Reach Water Quality Parameters 23 4.0 MODEL CALIBRATION AND CORROBORATION 26 4.1 Hydrology Calibration 26 4.2 Water Temperature Calibration 27 4.3 Water Quality Calibration 28 4.4 Model Corroboration Results 29 4.4.1 Water Temperature Corroboration 29 4.4.2 Water Quality Corroboration 30 5.0 MODEL SENSITIVITY 31 6.0 REFERENCES 34 TETRA TECH 1 Crooked Creek QUAL2K Model October 15, 2019 C.1 Stream Hydrology Measurements 43 C.2 Nutrient Sampling 44 C.3 Longitudinal Dissolved Oxygen 48 C.4 Diurnal Dissolved Oxygen 60 LIST OF TABLES Table 1. Existing permit limits for the wastewater treatment plants located along Crooked Creek 5 Table 2. Reach segmentation for Crooked Creek QUAL2K model 9 Table 3. Reach hydraulic model setup inputs 11 Table 4. Meteorological inputs data source summary 12 Table 5. Hourly inputs for air temperature, dew point temperature, and cloud cover 13 Table 6. Light and heat model setup inputs 14 Table 7. USGS flow conditions in adjacent Goose Creek watershed (flows in cfs) 16 Table 8. Headwater water quality initial model inputs (calibration model) 18 Table 9. Headwater water quality initial model inputs (corroboration model) 19 Table 10. Point source flow and water quality inputs (calibration period) 20 Table 11. Point source flow and water quality inputs (corroboration period) 21 Table 12. Tributary flow and water quality inputs (calibration model) 22 Table 13. Tributary flow and water quality inputs (corroboration model) 23 Table 14. Model inputs for bottom algae coverage 24 Table 15. Crooked Creek QUAL2K model sensitivity test runs 31 Table 16. Crooked Creek QUAL2K model sensitivity test run results 33 LIST OF FIGURES Figure 1. Crooked Creek watershed map 1 Figure 2. Crooked Creek QUAL2K model reach segmentation 2 Figure 3. Simulated and observed DO along Crooked Creek (calibration) 3 Figure 4. Simulated and observed DO along Crooked Creek (corroboration) 3 Figure 5. Crooked Creek watershed location map 2 Figure 6. Crooked Creek watershed elevation and reach map 2 Figure 7. Crooked Creek point source discharge locations and YPDRBA water quality sampling sites 4 CTETRA TECH 2 Crooked Creek QUAL2K Model October 15, 2019 Figure 8. LSPC model extent and subbasins for the Goose and Crooked Creek watersheds 7 Figure 9. Crooked Creek QUAL2K model reach segmentation 9 Figure 10. Crooked Creek summer 2016 cross sectional surveys by Tetra Tech 10 Figure 11. Crooked Creek channel bottom width measured from summer 2016 cross sections 11 Figure 12. Crooked Creek stream discharge estimates 16 Figure 13. Simulated and site-estimated flows for Crooked Creek model extent(calibration) 27 Figure 14. Simulated and observed water temperature along Crooked Creek (calibration) 28 Figure 15. Simulated and observed DO along Crooked Creek (calibration) 29 Figure 16. Simulated and observed water temperature along Crooked Creek (corroboration) 30 Figure 17. Simulated and observed DO along Crooked Creek (corroboration) 30 Figure 18. Sensitivity test results (runs 1 and 2): bottom algae coverage and SOD rate 32 Figure 19. Sensitivity test results (runs 3, 4, and 5): Manning's n, shade, and headwater flow 32 Figure 20. Sensitivity test results (run 6): reaeration model selection 33 ®TETRA TECH 3 1.0 INTRODUCTION Crooked Creek is a Class C waterway, with the South Fork, North Fork, and Crooked Creek downstream of the confluence all listed as Category 5 impaired waterways for turbidity and ecological/biological integrity (NC DENR, 2016). The Crooked Creek watershed is located largely in Union County, North Carolina with a small fraction of land in the headwaters located in Mecklenburg County. The watershed is on the southeastern extent of the Charlotte metropolitan area, immediately east of the City of Matthews. The North Fork and South Forks of Crooked Creek join north of the City of Monroe, then flow eastward as Crooked Creek until the confluence with Rocky River in the Yadkin Pee Dee River Basin (Figure 5). The Crooked Creek drainage area is about 50 square miles, and the mainstem of the creek currently receives effluent from three permitted wastewater treatment plants (WWTPs): Hemby Acres, Crooked Creek#2, and Grassy Branch. Elevation across the watershed ranges from 406—794 feet(124—242 meters) (Figure 6). The North Fork Crooked Creek is approximately 11.6 miles long, South Fork Crooked Creek is 13.9 miles long, Crooked Creek south of the confluence is 12.2 miles long, and the Grassy Branch tributary is 3.0 miles long. There are also several small unnamed tributaries within the watershed. In order to simulate existing conditions along Crooked Creek, a QUAL2K model was set up, calibrated and corroborated based on data collected in 2016. QUAL2K is a one-dimensional steady-state river water quality model frequently used for simulating DO (Chapra et al., 2012). QUAL2K assumes a well-mixed stream channel (both vertically and laterally), and employs a diel, or 24-hour period, heat budget which can be used to model DO on an hourly basis. Model calibration and corroboration used data collected during August and September 2016, along with supplemental data from other sources. This report details data sources, QUAL2K model setup, calibration, corroboration, and sensitivity analyses. 1 It TETRA TECH Crooked Creek QUAL2K Model October 15, 2019 North Carolina1 t Mecklenburg 1r I� County Rocky River Stanly County Crooked Creek Southparof a ._� ,X Union ^^ ��'-� /' County , Si 41*It 11 1111; .. / North Fork i ® ` ii 3 ' Crooked Creek riki :10 Grassy Branch , '-/110'4 .., , ' . I .1 .1N,‘ 411)*III4 ,......... AAilo Legend South Fork Stream/River Crooked Creek - Highway i Interstate RI / Watershed Boundary �� Crooked Creek Watershed N 0 075 ,5 3 County Boundary 7L TETRA TECH wc_ 'yo c�mRsaai ii-xi»�i kcnoua A�J o 07s sO ff--- 3 O State Boundary Miles Figure 5. Crooked Creek watershed location map ,Rocky River Stanly County Crooked Creek S Mecklenburg ' County UnionNI; (\r;S County / { 'North Fork Crooked Creek 101 ,ram- y'A ,� 4." , Grassy Branch tillirit ' '0\ Ste' '+ 440 � h ie Legend . aP South Fork Crooked Creek River/Stream =Watershed Boundary County Boundary • Elevation(feet) High 794 Crooked Creek Watershed N0 , taari Et TETRATECH Mortal Elevation Model d k, ta�Kan one Low 406 A3M.1e5 Figure 6. Crooked Creek watershed elevation and reach map TETRA TECH 2 Crooked Creek QUAL2K Model October 15, 2019 2.0 SUMMARY OF AVAILABLE DATA The available data related to flow and water quality in the Crooked Creek watershed prior to the summer of 2016 was relatively limited, therefore field work was conducted by Tetra Tech to provide directly applicable data required for QUAL2K model setup, calibration, and corroboration. Note that there are no USGS or other flow gaging stations present within the Crooked Creek watershed. Available data for Crooked Creek which is relevant to QUAL2K model development is provided below. 2.1 GOOSE AND CROOKED CREEKS LWP In 2008, the North Carolina Ecosystem Enhancement Program (NCEEP, now referred to as DMS which stands for Division of Mitigation Services) began development of a local watershed plan (LWP)for the Goose and Crooked Creek watersheds. The LWP involved preliminary characterization of the watersheds starting in 2008 and a more detailed watershed assessment starting in 2010. The LWP (Tetra Tech, 2012a) focused on: • Determining the functional status of aquatic systems in the watershed. • Identifying key stressors and their sources impacting water quality, habitat, and hydrology. • Determining where management to address sources and stressors is most needed. • Identifying potential management opportunities and key assets of the watershed. Data collection and analysis associated with the LWP were used to inform channel characterization. For example, there was extensive documentation associated with the channel bed materials, presence of snags and logs in the streambed, and anecdotal evidence informs decision making in the model such as the high instream Manning's n roughness values. 2.2 PERMITTED POINT SOURCE MONITORING There are three point sources present within the Crooked Creek watershed which are permitted through the National Pollutant Discharge Elimination System (NPDES). Hemby Acres WWTP (NPDES ID: NC0035041, permitted discharge 0.3 MGD) and Grassy Branch WWTP (NPDES ID: NC0085812, permitted discharge 0.05 MGD) are minor point sources, whereas Crooked Creek#2 WWTP (NPDES ID: NC0069841, permitted discharge 1.9 MGD) is classified as a major point source (Figure 7). Effluent discharge and instream monitoring data collected for these facilities was used to support model setup and calibration is presented in Appendix A. Carolina Water Service Inc., which owns and operates the Hemby Acres WWTP located on the North Fork of Crooked Creek, conducts instream water quality sampling immediately upstream and downstream of the effluent discharge location. Sampling at these locations approximately 200 feet upstream and 200 feet downstream of the outfall has been collected on a weekly basis since 2014 and consists of temperature, DO, and fecal coliform bacteria. Carolina Water Service, Inc. also reports treated effluent flow and water quality data associated with their permitted discharge: flow reported daily, while water temperature, pH, five-day biochemical oxygen demand (BOD5), ammonia (NH3), DO, and total suspended solids (TSS) are reported weekly. ®TETRA TECH 3 Crooked Creek QUAL2K Model October 15, 2019 .` Rocky River Stanly County * Crooked Creek Grassy Branch 0'$4. North Fork @ Crooked Creek WWTP(NC0085812) Crooked Creek Cre e k HembyAcresWWTP• WWTP02 t (NC0035041) ' MC0068841) 50 )ir ' @SR 1520Q8386200 �1 08388000)rip '7, , ____;\ ire, @SR 1514 _lit @ NC218 4 -. Grassy Branch AIIP A 7.it p* South Fork Legend Crooked Creek g WWTP Discharge Site Coalition Chemistry Station -- River/Stream N. Crooked Creek Watershed N o 05 , 2 n Watershed Boundary irk TETRA TECH Coalition Water Quality Sampling A oKaomerors A o os z County Boundary owes .s•oroe�..om,i 201eNNovae Figure 7. Crooked Creek point source discharge locations and YPDRBA water quality sampling sites Union County owns and operates the other two NPDES-permitted dischargers located along Crooked p Creek: major discharger Crooked Creek#2 WWTP and minor discharger Grassy Branch WWTP. Treated effluent flow is reported daily for both dischargers. Water temperature and pH are reported daily for weekdays only at both sites. BOD5, NH3, DO, and TSS are reported weekly for Grassy Branch and daily on weekdays for Crooked Creek#2. Chemical oxygen demand (COD) is reported monthly for both sites, and total nitrogen (TN), total phosphorus (TP), and hardness are reported monthly for Crooked Creek#2. Note that effluent sampling for Crooked Creek#2 occurs prior to entering a pipe that carries the effluent from the plant to the discharge location. The distance between the plant sampling point and the pipe outfall is approximately 2.5 miles, which raised concerns that DO depletion could occur during transit through the closed system. Tetra Tech's sampling of the effluent, however, showed that DO concentrations in the effluent leaving the pipe were similar to those recorded at the entrance to the pipe. The NPDES permit limits for the existing outfalls within the Crooked Creek watershed are detailed in Table 1. ®TETRA TECH 4 Crooked Creek QUAL2K Model October 15, 2019 Table 1. Existing permit limits for the wastewater treatment plants located along Crooked Creek. Permitted Allowable Flows and Concentrations (Summer) NPDES ID Facility Name Flow (MGD) BOD5(mg/I) NH3-N (mg/I) DO (mg/I) TSS (mg/I) NC0035041 Hemby Acres 0.3 9.0 3.0 >- 5.0 30.0 NC0069841 Crooked 1.9 5.0 2.0 ?6.0 30.0 Creek#2 NC0085812 Grassy Branch 0.05 5.0 2.0 >- 5.0 30.0 There is one additional permitted discharge located in the watershed, Radiator Specialty Company (NPDES ID NC0088838) which discharges near the headwaters of the South Fork Crooked Creek. This permit is associated with groundwater remediation and has a maximum allowable discharge of 0.09 MGD. This discharge is not simulated directly in the Crooked Creek QUAL2K model, however it is captured indirectly through the model inputs associated with the downstream end of the South Fork Crooked Creek. 2.3 YPDRBA (COALITION) INSTREAM SAMPLING There are four Coalition water quality sampling sites in the Crooked Creek watershed which are monitored by the Yadkin Pee Dee River Basin Association (YPDRBA). Of these four sites, two are located on the North Fork Crooked Creek (Q8386000, Q8386200), one is located on Crooked Creek below the confluence of the North and South Forks (Q8388900), and one is located below the confluence of Grassy Branch (Q8388000) (Figure 7). All four sites monitor temperature (temp), pH, DO, and total nitrogen (TN) approximately monthly, and Site Q8388000 also measures other nutrient data on a monthly basis since 2013 including nitrate and nitrite (NOX), ammonia (NH3), and total Kjeldahl nitrogen (TKN). These Coalition sites also monitor turbidity, fecal coliform bacteria, conductivity, and total suspended solids (TSS) on a monthly basis. These data were used to support model calibration to instream conditions along Crooked Creek and are presented in Appendix B. Note that sampling at site Q8388900 was discontinued during 2013. 2.4 TETRA TECH SAMPLING During the late summer of 2016, hydraulic and water quality sampling was performed by Tetra Tech on three separate field trips: August 15-19, August 31-September 2, and September 13-16. Sampling efforts included surveying 20 cross sections along Crooked Creek, estimating flow velocity and discharge, and generating a log of hydraulic information related to the creek. Water quality sampling on all three trips involved longitudinal DO sampling by probe, deployment of multi-day sondes for diurnal DO and water temperature fluctuation measurements, and grab sampling for water quality analyses for oxygen-related and nutrient-related constituents. The longitudinal samples included direct sampling of the effluent discharges, and a few small tributaries. The 2016 summer sampling results provided key data for model parameterization and calibration (Appendix C). CTETRA TECH 5 Crooked Creek QUAL2K Model October 15, 2019 2.5 HEC-RAS MODELING EFFORTS Two flow models have been created for the Crooked Creek watershed using the Hydrologic Engineering Center River Analysis System (HEC-RAS) model developed by the US Army Corps of Engineers (USACE, 2016). HEC-RAS models are used by hydraulic engineers for channel flow and stage analysis for floodplain determination, typically using design storm events. The combined HEC-RAS models cover the full extent of Crooked Creek, Grassy Branch, and the North and South Forks. Although HEC-RAS models are largely developed and applied for high-flow flood condition modeling, certain components of the models may be useful for low flow steady-state analysis, such as calibration of reach hydraulic parameters and constraining hydraulic parameterization. The HEC models in the Crooked Creek watershed covered all of the mainstem and major tributaries. Most of the HEC-RAS models were obtained from the NC Floodplain Mapping Program —Geospatial and Technology Management Dept. Several HEC-RAS models for portions of the Crooked Creek mainstem were provided by Union County. The HEC-RAS models comprise both "Limited Detail Study" and "Detailed Study" flood models. The"limited detail" models predict flood delineations for the 100-year storm event using cross section geometry developed from LIDAR data. The"detailed" models are much more rigorous than "limited detail" studies because they determine specific channel profiles, bridge and culvert opening geometry, and floodplain characteristics using traditional field surveys. The "detailed study" model also includes flood profiles for the 10-, 25-, and 50-year storm events. 2.6 GOOSE AND CROOKED CREEK LSPC MODEL A model was developed to simulate hydrology and water quality in the Goose and Crooked Creek watersheds in support of watershed planning conducted by NCEEP, Centralina Council of Governments and North Carolina Division of Water Quality (Tetra Tech, 2012b). This effort involved simulating these two adjacent drainages using the Loading Simulation Program C++ (LSPC) watershed model to represent existing conditions (Tetra Tech, 2009a). The LSPC model, a continuous watershed model with a 1-D stream channel representation, was parameterized based on hydrologic soil groups, land slope characteristics, and land use/land cover across the two basins. Hydrology was calibrated to observed streamflow at multiple locations within the Goose Creek watershed. Although there are no flow monitoring stations within the Crooked Creek basin (and no direct hydrology calibration), the geology and soils of Crooked Creek are similar to Goose Creek. As a result, model hydrology predictions are likely reasonable across a range of flows. Water quality calibration was performed for both creeks by comparing simulated pollutant concentrations and loads to observed values. CTETRA TECH 6 Crooked Creek QUAL2K Model October 15, 2019 At 104 110 103 lie -'11 t 05 _ s 201 108 204 202 106 205 203 216-\- 206 / 2lilt / 210 *07 Legend LSPC Model Reach 209 n LSPC Model Subbasn ICrooked Creek Watershed Crooked Creek Watershed N - s 2 I I Goose Creek Watershed TFTRA TECH LSPC Model Extent ,„ tv M�I�e County Boundary Figure 8. LSPC model extent and subbasins for the Goose and Crooked Creek watersheds ®TETRA TECH 7 Crooked Creek QUAL2K Model October 15, 2019 3.0 QUAL2K MODEL SETUP 3.1 MODEL DOCUMENTATION The most recent version of the QUAL2K model available at the time of this report was used for modeling Crooked Creek: QUAL2K version 2.12b1. QUAL2K is a river and stream water quality model that is intended to represent a modernized version of the QUAL2E model (Brown and Barnwell, 1987). QUAL2K was developed at Tufts University and has been funded partly by the United States Environmental Protection Agency (Chapra et al., 2012). 3.2 MODEL DATE SELECTION The QUAL2K model is set up to run for a specific date, and information about latitude, longitude, and time zone are used to inform solar energy forcing. Based on the summer 2016 sampling, the QUAL2K model for Crooked Creek was setup and calibrated to a date in August which best represented the first two sampling trips. The model was corroborated as well by comparing the simulated and observed results associated with the third sampling trip in September. The first and second trips to the Crooked Creek area for data collection were August 15— 19, and August 31 —September 2. Grab samples were taken on those sampling efforts for the most part on August 16 and August 31 respectively. A date chosen approximately halfway between those two dates was identified to use as the model calibration date (August 24, 2016). The model corroboration date was chosen as the grab sampling date of September 14, 2016 during the third sampling field trip which was September 13 —September 16. There is reasonable justification for combining the first and second field trips into a single calibration period based on known flow and atmospheric conditions. An analysis of flow gages in the adjacent watershed of Goose Creek, as well as an analysis of local air temperatures suggest that conditions on the August 16 and 31 were sufficiently alike to support combining data associated with those two trips for a single steady state model calibration run. Average air temperature on 8/16 and 8/31 were 84.6 °F (29.2 °C) and 79.4 °F (26.3 °C) respectively. The two USGS flow gages along Goose Creek (0212467451 and 0212467595) both observed streamflow conditions between 0.4 and 0.9 cfs on August 16th and 31st Flows at these gages experienced average annual flows in 2016 on the order of 7.0 and 4.4 cfs respectively, so conditions were considered sufficiently similar and relatively low during the two August dates compared to the annual statistics. 3.3 MODEL SEGMENTATION The extent of the Crooked Creek QUAL2K model is defined as upstream of the Hemby Bridge VWVfP on the North Fork, running 21.0 miles (33.8 kilometers) to the outlet at Rocky River. The total modeled distance is subdivided into "reaches" which themselves are made up of 0.1-kilometer computational "elements". In general reach divisions represent areas of approximately similar hydraulic conditions. For Crooked Creek, the 6 segmented reaches largely reflect key points of interest in the watershed such as VVVVTP discharges or tributary inflows. The reach located downstream from the South Fork Crooked Creek (SFCC) confluence is segmented at a large beaver dam above Highway 601 because this stretch is particularly obstructed and sluggish due a series of large beaver/debris dams. This reach between SFCC and the end of the beaver dams above Highway 601 has significant hydrologic differences than downstream of the dams, reflected in channel geometry, flow velocity, and observed DO concentrations. TETRA TECH 8 -.O Crooked Creek QUAL2K Model October 15, 2019 Hydraulic parameterization for each model reach was based on GIS-based spatial analyses of NHDPlusV2 flowlines, a 3-meter resolution digital elevation model (DEM) obtained from the USDA Data Gateway, and field data from surveys conducted in August and September 2016. Table 2 and Figure 6 summarize the reach segmentation for the Crooked Creek QUAL2K model which were used for model setup and did not vary between calibration and corroboration model setups. Table 2. Reach segmentation for Crooked Creek QUAL2K model Reach Upstream Downstream Reach Description Length, Elevation, Elevation, mi (km) ft(m) ft(m) 1 Headwaters to Hemby Bridge WWTP 0.88 (1.42) 623 (190) 617 (188) 2 Hemby Bridge WWTP to Crooked Creek#2 2.80 (4.50) 617 (188) 587 (179) WWTP 3 Crooked Creek#2 WWTP to South Fork 3.75 (6.03) 587 (179) 558 (170) Crooked Creek (SFCC) confluence 4 South Fork Crooked Creek (SFCC) to end of 1.61 (2.59) 558 (170) 551 (168) two large beaver dams 5 End of beaver dams, crossing Highway 601, to 5.21 (8.39) 551 (168) 502 (153) Grassy Branch WWTP 6 Grassy Branch WWTP to Rocky River 6.72 (10.82) 502 (153) 410 (125) •Rocky River 1 Crooked Creek `t Grassy Branch WTP\ ,;a~•. W 'N Hemby Acres WWTP North Fork Crooked Creek. ' a Crooked Crooked Creek WWTP#2• ---\._/ - _ ` Grassy Branch r fr 1 lAbdr PM i Legend .� 1 WWTP Discharge • A Large Beaver Dam f South Fork Crooked Creek - RiverlStream OWatershed Boundary Model Reach } Ream, / Reach 2 ,'\ — Reach 9 .�Reach• Crooked Creek Watershed N c :` - 2 ._Ream 6 (,l TETRA TECH QUAL2K Model Segmentation OKdomerera ll 11 �� Reach 6 Figure 9. Crooked Creek QUAL2K model reach segmentation OTETRA TECH 9 Crooked Creek QUAL2K Model October 15, 2019 3.4 REACH HYDRAULICS Stream hydraulics were simulated using the Manning's Formula method within QUAL2K. Model inputs related to Manning's Formula may vary for each reach and are represented as average conditions based on the 2016 field survey cross sectional data (Figure 10). There were 20 locations surveyed during summer 2016, and channel geometry characteristics are used to approximate average conditions for each model reach. There is a strong relationship between increasing channel bottom width and distance from the headwaters, reflecting the corresponding increase in drainage area and flow; therefore, the average distance of each reach from the headwaters was used to approximate channel bottom width (Figure 11). Surface and bottom channel widths were used to estimate average channel side slopes for each reach by assuming trapezoidal area. Rocky River Crooked Creek 0 0 0 '• • North Fork Crooked Creek 0 4 0 Grassy Branch Pob Legend 0 Cross Section Site River/Stream South Fork Crooked Creek OWatershed Boundary Model Reach - Reach 1 Reach 2 ,` Reach J \� .......� Reach 4 Crooked Creek Watershed N 0 05 1 2 Reach lb TETRA TECH 2016 Survey Cross Sections A oK4ometers 0 O S 1 2 Reach 6 .e., yozoY a.:no`.auc OMiles Figure 10. Crooked Creek summer 2016 cross sectional surveys by Tetra Tech IN TETRA TECH 1 0 Crooked Creek QUAL2K Model October 15, 2019 30 y=0.9833x+1.764 R2=0.7034 a 25 • • 20 0 •Reach 1(no data) • �. •Reach 2(5 sites) o 15 • • • *Reach 3(3 sites) m • • • , 10 • •Reach 4(No Data) •• •Reach 5(6 sites) 5 ?i • r' •Reach 6(6 sites) 0 0 5 10 15 20 Distance from headwaters (miles) Figure 11. Crooked Creek channel bottom width measured from summer 2016 cross sections For reach hydraulics, bottom channel widths were estimated based on the regression presented in Figure 11. Channel side slopes were estimated using surface and bottom channel widths and an average depth of 1 foot(0.32 meters). Bottom widths were generally small, and since water depths were shallow along the entire Crooked Creek, side slopes are high. Channel bed slope is calculated as the difference in upstream and downstream elevation divided by the reach length (refer to Table 1 for raw data). Manning's n (roughness coefficient) can range from about 0.025-0.150 for natural streams (Chow, 1959). Manning's n may be subject to alteration during model calibration because channel roughness is heavily influenced by pool-riffle structures, debris, and obstructions (Beven et al., 1979). Manning's n was initialized for all reaches as 0.1 which indicates "mountain streams with boulders" since there is significant data suggesting high debris content and irregular channel bottoms along the entire stream (Chow, 1959). Manning's n was the only reach hydraulic parameter adjusted during model calibration. Table 3. Reach hydraulic model setup inputs Reach Location Shorthand Channel Manning's Bottom Width, Side Bed Slope n ft(m) Slopes 1 HW to Hemby WWTP 0.0014 0.1 2.17 (0.66) 4.37 2 Hemby WWTP to CC#2 WWTP 0.0010 0.1 4.00 (1.22) 4.71 3 CC#2 WWTP to SFCC 0.0015 0.1 7.43 (2.26) 5.35 4 SFCC to Beaver Dams 0.0006 0.1 10.50 (3.20) 5.93 5 Beaver Dams to Grassy WWTP 0.0014 0.1 13.58 (4.14) 6.51 6 Grassy WWTP to outlet 0.0020 0.1 19.11 (5.83) 7.55 ®TETRA TECH 11 Crooked Creek QUAL2K Model October 15, 2019 3.5 METEOROLOGICAL INPUTS, LIGHT AND HEAT 3.5.1 Hourly Inputs Metrological inputs to the QUAL2K model include air temperature, dew point temperature, wind speed, cloud cover percentage, and percent of solar radiation blocked by stream shade. Hourly meteorological data are available through the Weather Underground (www.wunderground.com)for sites near Crooked Creek. The "Campobello Drive" site in Unionville, North Carolina (KNCUNION2) is located near Crooked Creek and was identified as the best source of hourly meteorological inputs for the QUAL2K model. For development of each meteorological input, see Table 4. Average air temperature as developed for model calibration was 83.1 °F (28.4 °C)with a daily range between minimum and maximum air temperatures of 15.95 °F (8.86 °C). Average air temperature as developed for model corroboration was 86.0 °F (24.6 °C) with a daily range between minimum and maximum air temperatures of 18.0 °F (10.0 °C). Table 4. Meteorological inputs data source summary Parameter Processing Note Air Hourly air temperatures (dry bulb temperatures) were calculated as hourly averages of Temperature data from the KNCUNION2 site on 8/16/2016 and 8/31/2016 for the calibration model. Hourly air temperature from the same station was used from 9/14/2016 for the corroboration model. Inputs did not vary by reach. Dew Point Hourly dew point temperatures were calculated as hourly averages of data from the Temperature KNCUNION2 site on 8/16/2016 and 8/31/2016 for the calibration model. Hourly dew point temperatures from the same station was used from 9/14/2016 for the corroboration model. Inputs did not vary by reach. Wind Speed Hourly wind speed was available from the KNCUNION2 site, however the riparian vegetation and channel incision shelters the stream so significantly (as observed during field trips)that wind was assumed to be negligible to the stream for both calibration and corroboration models. Inputs were set to zero for all hours at all reaches. Cloud Cover Hourly cloud cover were calculated as hourly averages of data on 8/16/2016 and 8/31/2016 from the closest regional airport(Monroe Airport, station ID: KEQY). Hourly cloud cover from the same station was used from 9/14/2016 for the corroboration model. Inputs did not vary by reach. Shade A single shade percentage of 70% is applied to all hours and all reaches as an average daily approximation for both calibration and corroboration models. Note that Crooked Creek is highly shaded, with much of the stream completely sheltered by vegetation such that the channel cannot be identified through aerial imagery. ®TETRA TECH 12 Crooked Creek QUAL2K Model October 15, 2019 Table 5. Hourly inputs for air temperature, dew point temperature, and cloud cover Calibration Model Corroboration Model Hour Air Temp Dew Point Cloud Air Temp Dew Point Cloud (°F) Temp (°F) Cover(%) (°F) Temp (°F) Cover(%) 1 78.75 68.42 0.00% 72.67 66.00 0.00% 2 77.75 67.90 0.00% 71.33 65.00 0.00% 3 76.81 68.13 0.00% 70.17 64.17 0.00% 4 76.20 68.00 0.00% 69.33 64.00 41.67% 5 75.56 68.00 0.00% 69.00 63.50 45.83% 6 74.90 68.00 0.00% 68.00 63.00 50.00% 7 74.30 67.50 0.00% 68.00 63.00 93.75% 8 77.60 70.80 0.00% 68.17 63.33 100.00% 9 81.55 72.25 0.00% 70.00 65.50 100.00% 10 85.50 73.70 31.25% 72.67 68.33 100.00% 11 86.00 74.40 37.50% 75.83 71.33 91.67% 12 88.10 75.80 62.50% 78.00 72.67 25.00% 13 89.60 76.00 50.00% 79.83 73.00 0.00% 14 90.00 75.62 62.50% 81.60 72.40 0.00% 15 89.67 74.80 50.00% 84.00 70.83 0.00% 16 90.25 74.25 0.00% 85.50 70.00 0.00% 17 89.83 74.33 12.50% 86.00 70.00 0.00% 18 89.67 74.33 0.00% 86.00 68.00 50.00% 19 89.38 73.88 0.00% 84.40 69.00 0.00% 20 87.60 72.40 0.00% 82.20 68.20 0.00% 21 84.58 70.90 0.00% 79.33 67.00 0.00% 22 82.20 69.90 0.00% 77.25 67.00 0.00% 23 80.46 69.16 0.00% 75.60 67.00 0.00% 24 79.13 69.00 0.00% 74.60 66.40 0.00% OTETRA TECH 13 Crooked Creek QUAL2K Model October 15, 2019 3.5.2 Light and Heat Inputs Several parameters related to light and heat functions can be adjusted for a given QUAL2K model. For model setup, solar inputs are calculated within the model based on latitude, time zone, and Julian day. Based on these inputs for Crooked Creek on 8/24/2016, sunrise and sunset were calculated within the model to be at 6:48 AM and 7:58 PM, which were externally verified through the North Carolina Wildlife Resources Commission, which publicly documents sunrise and sunset times across North Carolina (www.NCWildLife.org). Sunrise and sunset times for the corroboration model on 9/14/2016 were calculated in the model as 7:04 AM and 7:29 PM respectively. Most light and heat parameters were estimated based on suggested values from the QUAL2K manual. There are a number of options for modeling atmospheric attenuation of solar energy, atmospheric longwave emissivity, and wind speed function for evaporation and air convection/conduction, and sediment heat parameters (Table 6). Table 6. Light and heat model setup inputs Parameter(units) Model Input Note Light Parameters Photosynthetically Available Radiation 0.47 Light parameters initialized based on Background light extinction (/m) 0.2 QUAL2K example file. Linear chlorophyll light extinction (/m) 0.0088 Nonlinear chlorophyll light extinction (/m) 0.054 ISS light extinction (/m) 0.052 Detritus light extinction (/m) 0.174 Model Parameters Atmospheric attenuation model for solar Bras Default atmospheric formula for QUAL2K Atmospheric turbidity coefficient 2 Default value suggested by QUAL2K Manual Atmospheric longwave emissivity model Brutsaert This equation tends to allow for warmer water temperatures to be achieved Wind speed function for evaporation and Brady- Default wind speed function for QUAL2K air convention Graves-Geyer Sediment Heat Parameters Sediment thermal thickness (cm) 20 Model default suggestions from QUAL2K Sediment thermal diffusivity (cm2/s) 0.005 manual. Default suggestion for sediment thermal thickness of 10 cm was modified Sediment density (g/cm3) 1.6 to 20 cm given the observed presence of Sediment heat capacity (cal/g °C) 0.4 thicker sediment along the channel. TETRA TECH 14 Crooked Creek QUAL2K Model October 15, 2019 3.6 CARBONACEOUS BIOCHEMICAL OXYGEN DEMAND SIMULATION The QUAL2K model simulates instream chemical biological oxygen demand (CBOD) as two different pools: fast CBOD which is rapidly oxidized and labile in nature, and slow CBOD which is slowly oxidized and refractory in nature. For the QUAL2K model of Crooked Creek, fast CBOD was used to simulate the presence of oxygen-demanding substances in WWTP effluent, while slow CBOD was used to simulate the presence of instream background decay of organic matter such as leaf litter. The QUAL2K manual suggests that when modeling slow and fast CBOD separately, to keep the distinct pools apart by setting the CBOD hydrolysis rate to zero, so that choice was made for the Crooked Creek model. Incubation time for BOD or CBOD measurements in laboratories is typically short-term for five days, reporting the results as BOD5 or CBOD5 respectively. These five-day concentrations of BOD and CBOD must be converted to the ultimate concentration of CBOD (CBODuitimate)for simulation in QUAL2K in order to approximate the slow or fast CBOD concentration after some fifty days of decomposition. For slow CBODuitimate simulation in the model the Phelps equation below may be employed, as detailed in the QUAL2K manual (Chapra et al., 2012): CBOD5 slow CBODuitimate — 1 — e(—klx5) Note that for the equation above, ki is the rate of oxidation for CBOD which the QUAL2K manual suggests can range from 0.05—0.3/d. For slow CBODuitimate in the model, 0.05 /d will be used, and for fast CBODultimate, 0.3/d will be used in the model environment. As mentioned above, WWTP effluent was modeled as fast CBODultimate, which was based on Discharge Monitoring Report (DMR) data reported as BOD5 concentrations. The original QUAL-II model (NCASI, 1985) internally converted 5-day BOD to ultimate CBOD using a ratio of 1.46 and was not user-specified (EPA, 1985). Studies have shown that rates can vary significantly from low ratios for domestic wastewater to very high ratios (e.g., 30) for pulp and paper waste (EPA, 1985). Leo, et al. (1984) summarized the results for numerous facilities that showed the ratios for secondary to advanced secondary averages from slightly below to slightly above 2. In the absence of specific lab studies on the existing County plant effluent BOD5 to CBODultimate ratio, a factor of 2 was assumed: fast CBODuitimate = 2 x BOD5 In summary, boundary conditions for headwaters and tributaries were simulated as slow CBOD pools estimated based on in-stream CBOD5 sampling and Phelps first-order reaction equation, while boundary conditions for effluent point sources were simulated as fast CBOD pools estimated based on DMR BOD5 sampling and a ratio of 2:1 for BOD5:CBODultimate. 3.7 BOUNDARY CONDITIONS 3.7.1 Headwaters 3.7.1.1 Headwater Flows Of the twenty stream cross-sections surveyed during summer 2016, ten were paired with velocity measurements to estimate instantaneous streamflow. Stream velocity during each of three separate sampling trips was so low that a propeller-driven Global Water FP111 Flow Probe velocity meter with a lower measurement limit 0.3 ft/s (0.1 m/s) was not able to provide an estimate (i.e., velocity was too low to fril TETRA TECH 15 Crooked Creek QUAL2K Model October 15, 2019 move the propeller to measure velocity). Therefore, at these ten sites, an orange was timed to float a specific distance a crude but reasonable way to estimate average channel velocity. Stream discharge was subsequently approximated at these ten sites by multiplying the estimated flow velocity by cross- sectional area (Figure 12). This estimation was conducted using a linear regression of eight of the sites, as two were deemed to be probable outliers and may reflect error in methodology. 7 6 y=0.1713x+1.2151 R2=0.8221 r `- •Reach 1(No Data) • 2 sites•Reach 2 4 ( ) •Reach 3(2 sites) • 3 • •Reach 4(No Data) • •Reach 5(3 sites) 2 t' •Reach 6(1 site) 1 •Outliers(Reach 3,6) • 0 0 5 10 15 20 Distance from headwaters (miles) Figure 12. Crooked Creek stream discharge estimates Although there are no flow gages located along Crooked Creek, flow gages in the adjacent Goose Creek watershed during the summer 2016 sampling period revealed that reasonably similar low-flow conditions were present during all three sampling trips. Streamflow conditions at USGS gages 0212467451 (Goose Creek at SR1524 near Indian Trail) and 0212467595 (Goose Creek at SR1525 near Indian Trail) were reported to be similarly low during all summer sampling trips in Crooked Creek (Table 7). Based on the limited flow data in-hand and the low-flow conditions in the adjacent Goose Creek, it is assumed that flow conditions were reasonably similar across all three sampling trips to use the same flow boundary conditions during calibration and corroboration model periods. Table 7. USGS flow conditions in adjacent Goose Creek watershed (flows in cfs) USGS gage Minimum Maximum Average Flow on Flow on Flow on Flow, 2016 Flow, 2016 Flow, 2016 8/16/2016 8/31/2016 8/14/2016 0212467451 0.38 98.44 4.46 0.61 0.38 0.48 0212467595 0.62 158.78 7.01 0.94 0.78 0.79 It is possible to use the relationship between discharge and distance from the headwaters to approximate flows at the headwaters. As seen in Figure 12 and using the linear regression, the best estimate of headwater flow conditions during the entire summer sampling period of 2016 is 1.215 cfs (0.034 cms). 16 "Et TETRA TECH Crooked Creek QUAL2K Model October 15, 2019 3.7.1.2 Headwater Water Quality Water quality conditions at the headwaters to be assumed for model calibration and corroboration periods were developed from the sampling sites located upstream of the Hemby Acres WWTP. Water temperature and DO were observed by Carolina Water Services Inc. upstream of the WWTP on a weekly basis. For the calibration period, the average of conditions from the weeks of the associated trips 1 and 2 were used to generate average headwater conditions for water temperature and DO, while grab sample site#1 results were averaged for trip 1 and trip 2 for all other applicable constituents. For the corroboration period, average conditions used during field trip 3 as sampled upstream of Hemby Acres WWTP were used in tandem with grab sampling at site#1. Headwater water quality inputs for model initialization for the calibration period and corroboration period are detailed in Table 8 and Table 9 respectively. Headwater boundary conditions specified for the calibration and corroboration periods are not subject to change although they vary between the two periods based on instream data. Within the model, the downstream extent was not a prescribed boundary. For the simulation of CBODuitimate at the headwaters, the entire pool was estimated to be slow CBOD because upstream of this point does not include any effluent sources. Modeled slow CBOD is approximated as a function of observed CBOD5 at WQ Grab Site#1 and the slow decay rate detailed in Section 3.6 of 0.05/d. Measurements of CBOD5 at Site#1 on field trips 1, 2, and 3 were all non-detects (detection limit of 2 mg/I), therefore estimates of instream CBOD5 were set to half the detection limit for the calculation of ultimate slow CBOD to use for model input for both calibration and corroboration: CBOD5 CBODuitimate — 1 — e(_klx5) mg mg slow CBOD at headwaters = 1 _e� o os/a)<5 = 4.52 meµ'TETRA TECH 17 Crooked Creek QUAL2K Model October 15, 2019 Table 8. Headwater water quality initial model inputs (calibration model) Parameter Model Input Data Source Water Temperature (°F) 74.8 Average of upstream of Hemby WWTP samples on 8/18/16 (76.3 °F) and 8/30/16 (73.4 °F) Conductivity (pmhos) 252 Unknown at headwaters, set to average result of all downstream sondes from Trip 2 (no data from Trip 1) Inorganic Solids (mg/L) 0 Unknown at headwaters, assume zero Dissolved Oxygen (mg/L) 4.38 Average of upstream of Hemby WWTP samples on 8/18/16 (4.43 mg/I) and 8/30/16 (4.32 mg/I) Slow CBOD (mg/L) 4.52 Refractory pool of CBOD calculated based on instream Fast CBOD (mg/L) 0 CBOD5 measurements from WQ Grab Site#1 on Trips 1 and 2 Organic Nitrogen (pg/L) 508 Calculated as the difference between Trip 1 and Trip 2 observed TKN and NH3 for WQ Grab Site#1; non- detects set to half of the detection limit. NH4-Nitrogen (pg/L) 25 Ammonia was not detected in the headwaters from WQ Grab Site#1 from Trips 1 and 2, therefore the headwaters were set to half of the detection limit. NO3-Nitrogen (pg/L) 280 Average of observed NOX at WQ Grab Site#1, Trips 1 and 2. Inorganic Phosphorus (pg/L) 95 Observed PO4 from WQ Grab Site#1 was used from Trip 2. The observation from Trip 1 was not used as it was flagged for quality control exceedances. Organic Phosphorus (pg/L) 16 Difference between Trip 1 and Trip 2 observed TP and PO4 for WQ Grab Site#1, excluding flagged PO4 sample. Alkalinity (mg/L) 100 Unknown at headwaters, use model default Phytoplankton (mg/L) 0 Unknown at headwaters, assume zero pH 7 Unknown at headwaters, use model default TETRA TECH 18 Crooked Creek QUAL2K Model October 15, 2019 Table 9. Headwater water quality initial model inputs (corroboration model) Parameter Model Input Data Source Water Temperature (°F) 71.8 Observed upstream of Hemby WWTP samples on 9/12/16 Conductivity (pmhos) 311 Unknown at headwaters, set to average result of all downstream sondes from Trip 3 Inorganic Solids (mg/L) 0 Unknown at headwaters, assume zero Dissolved Oxygen (mg/L) 3.63 Observed upstream of Hemby WWTP samples on 9/12/16 Slow CBOD (mg/L) 4.52 Refractory pool of CBOD calculated based on instream Fast CBOD (mg/L) 0 CBOD5 measurements from WQ Grab Site#1 on Trip 3 Organic Nitrogen (pg/L) 680 Calculated as the difference between Trip 3 observed TKN and NH3 for WQ Grab Site#1; non-detects set to half of the detection limit. NH4-Nitrogen (pg/L) 50 Ammonia was not detected in the headwaters from WQ Grab Site#1 from Trip 3, therefore the headwaters were set to half of the detection limit. NO3-Nitrogen (pg/L) 77 Observed NOX at WQ Grab Site#1 from Trip 3 Inorganic Phosphorus (pg/L) 51 Observed PO4 from WQ Grab Site#1 from Trip 3 Organic Phosphorus (pg/L) 69 Difference between Trip 3 observed TP and PO4 for WQ Grab Site#1 Alkalinity (mg/L) 100 Unknown at headwaters, use model default Phytoplankton (mg/L) 0 Unknown at headwaters, assume zero pH 7 Unknown at headwaters, use model default 3.7.2 Point Source Flows and Water Quality The three permitted wastewater treatment plant effluent dischargers along Crooked Creek were modeled explicitly: Hemby Acres WWTP which is operated by Carolina Water Services Inc., and Crooked Creek#2 WWTP and Grassy Branch WWTP which are both operated by Union County. For the most part, point source model inputs for flow and water quality were based on average conditions for August (calibration model) and average conditions for September(corroboration model) based on Discharge Monitoring Report (DMR) data. For parameters not available through DMR monitoring, concentrations were estimated based on grab samples from the discharge pipe outfalls from trips 1, 2, and 3 (Table 10, Table 11). DMR reports show that discharge flows and water quality did not vary widely across August and September. As detailed in Section 3.6, effluent fast CBOD pools estimated based on DMR BOD5 sampling and a ratio of 2:1 for BODs:CBODwtimate. When DMR-reported concentrations for any given parameter were listed as f TETRA TECH 19 Crooked Creek QUAL2K Model October 15, 2019 below detection limit, the concentration was assumed to be half of the detection limit for the purposes of calculating average effluent concentrations. Table 10. Point source flow and water quality inputs (calibration period) Hemby Acres Crooked Creek Grassy Branch Parameter WWTP #2 WWTP1 WWTP Discharge Information NPDES Permit ID NC0035041 NC0069841 NC0085812 Permit Class Minor Major Minor NPDES Permitted Flow(MGD) 0.3 1.9 0.05 Model Inputs based on DMR data (August 2016 Averages) Location (km), distance from outlet 32.48 27.81 10.82 Inflow(m3/s), [MGD] 0.0039 [0.09] 0.0364 [0.83] 0.0018 [0.04] Water Temperature (°F) 78.1 79.9 78.3 Dissolved Oxygen (mg/L) 6.5 7.6 7.7 Slow CBOD (mg/L) 0 0 0 Fast CBOD2 (mg/L) 8.36 2.38 3.60 Inorganic Suspended Solids (mg/L) 1.25 1.56 2.46 Ammonia Nitrogen (pgN/L) 50 940 640 pH 7.5 7.3 7.3 Model Inputs based on summer grab sampling data (Trips 1 and 2 Averages) Corresponding Grab Sample ID #2 #4 #12 Organic Nitrogen (NgN/L)3 565 1,100 825 Nitrate+ Nitrite Nitrogen (pgN/L) 38,000 28,450 39,000 Organic Phosphorus (pgP/L)4 800 2,000 1,150 Inorganic Phosphorus (pgP/L) 3,300 2,700 1,850 Specific Conductance (pmhos)6 641 628 837 Phytoplankton (ug/L) No Data, assume 0 Alkalinity (mg/L) 86.05 73.4 98.6 'Measurements were observed at the entrance of the pipe. DO measurements at the end of the pipe suggest that water quality does not change significantly through the pipe. 2easured and reported BOD5 was converted to fast CBODui imate as described in the text with 1:2 ratio. 'Organic nitrogen was not measured directly, but calculated as the difference between measured TKN and NH3 "Organic phosphorus was not measured directly, but calculated as the difference between measured TP and POa 'Alkalinity was not measured at Hemby Acres,so it was approximated as the average the other two dischargers 'Conductance measured from Trip 3(used for calibration and corroboration models) TETRA TECH 20 O Crooked Creek QUAL2K Model October 15, 2019 Table 11. Point source flow and water quality inputs (corroboration period) Hemby Acres Crooked Creek Grassy Branch Parameter WWTP #2 WWTP1 WWTP Model Inputs based on DMR Data (September 2016 Averages) Location (km), distance from outlet 32.48 27.81 10.82 Inflow(m3/s), [MGD] 0.0039 [0.09] 0.0381 [0.87] 0.0018 [0.04] Water Temperature (°F) 75.6 75.6 76.3 Dissolved Oxygen (mg/L) 6.8 8.0 7.6 Slow CBOD (mg/L) 0 0 0 Fast CBOD2 (mg/L) 11.80 4.08 2.00 Inorganic Suspended Solids 1.25 4.71 1.27 (mg/L) Ammonia Nitrogen (pgN/L) 50.00 57.06 255.56 pH 7.3 7.1 7.1 Model Inputs based on summer grab sampling data (Trip 3) Corresponding Grab Sample ID #2 #4 #12 Organic Nitrogen (pgN/L)3 1075 1875 100 Nitrate+ Nitrite Nitrogen (pgN/L) 25100 33900 53300 Organic Phosphorus (pgP/L)4 1600 1300 200 Inorganic Phosphorus (pgP/L) 4000 4800 4500 Specific Conductance (pmhos) 641 628 837 Phytoplankton (ug/L) No Data, assume 0 Alkalinity (mg/L) 64.65 37.7 91.4 'Measurements were observed at the entrance of the pipe. DO measurements at the end of the pipe suggest that water quality does not change significantly through the pipe. 2Measured and reported BOD5 was converted to fast CBODunimate as described in the text with 1:2 ratio. 3Organic nitrogen was not measured directly,but calculated as the difference between measured TKN and NH3 ^Organic phosphorus was not measured directly,but calculated as the difference between measured TP and PO4 'Alkalinity was not measured at Hemby Acres,so it was approximated as the average the other two dischargers ®TETRA TECH 21 Crooked Creek QUAL2K Model October 15, 2019 3.7.3 Tributary Flows and Water Quality Model inputs for flow and water quality for the South Fork Crooked Creek and Grassy Branch tributaries contributing to the Crooked Creek mainstem were developed based on a combination of observed data, water balance calculations, and best professional judgement. Streamflow was estimated at several points along Crooked Creek based on cross-section surveys paired with velocity measurements. By combining the observed streamflow information with the reported point source discharge data, the relative contributions of each modeled tributary can be estimated using a water balance assuming no other losses due to evaporation and groundwater seepage. For tributary inflows, CBOD is modeled as slow CBODunimate and estimated the same way as the headwaters. Table 12. Tributary flow and water quality inputs (calibration model) Grassy Parameter SFCC Branch Data Source Information Inflow, ft3/s (m3/s) 1.06 0.32 Estimated by water balance as the difference between (0.03) (0.009) instream flow estimates which are not accounted for by point source flows. Water Temperature, (°F) 81.86 74.48 Water temperature is based on probe sampling conducted on Trip 1 for SFCC and Grassy Branch. Note that Grassy Branch is cooler because it is largely groundwater-fed. Conductivity (pmhos) 252 252 No available it ble data, assumed same as headwaters ISS (mg/L) 0 0 No available data, assumed zero Dissolved Oxygen 2.47 2.67 DO estimates are based on probe sampling conducted on (mg/L) Trip 1 for SFCC and Grassy Branch. Alkalinity (mg/I) 100 100 No available data, assume model default Phytoplankton (ug/I) 0 0 No available data, assumed zero pH 7.35 6.23 pH estimates are based on probe sampling conducted on Trip 1 for SFCC and Grassy Branch. Slow CBOD (mg/L) 4.52 23.73 Average measured CBOD5 from Trips 1 and 2 was used to Fast CBOD (mg/L) 0 0 approximate slow CBOD as described in the text. Observed CBOD5 along Grassy Branch was noticeably high. Ammonia N (pgN/L) 478 25 NH3 and NOX data are averages of observed data from Organic N (pgN/L) 1,073 435 Trips 1 and 2 at WQ Site#9 (SFCC) and WQ Site#13 (Grassy Branch). Organic N was calculated as the Nitrate+Nitrite N (pgN/L) 2,865 1,600 difference between observed TKN and NH3 data. Organic P (pgP/L) 380 98 Organic P was calculated as the difference between Inorganic P (pgP/L) 245 72 observed TP and PO4 during Trips 1 and 2 for SFCC (WQ Site#9). Model inputs for Grassy Branch are from Trip 3 only because of a lab issue with P-species data from Trips 1 and 2 (WQ Site#13). TETRA TECH 22 ', Crooked Creek QUAL2K Model October 15, 2019 Table 13. Tributary flow and water quality inputs (corroboration model) Grassy Parameter SFCC Branch Data Source Information Inflow, ft3/s (m3/s) 1.06 0.32 Estimated to be the same as during the calibration period. (0.03) (0.009) Water Temperature (°F) 71.6 76.8 Water temperature is based on probe sampling conducted on Trip 3 for SFCC and Grassy Branch. Conductivity (pmhos) 102 263 Estimates are based on probe sampling conducted on Trip 3 for SFCC and Grassy Branch. ISS (mg/L) 0 0 No available data, assumed zero Dissolved Oxygen 2.47 2.67 DO estimates are based on probe sampling conducted on (mg/L) Trip 1 for SFCC and Grassy Branch. Alkalinity (mg/I) 100 100 No available data, assume model default Phytoplankton (ug/I) 0 0 No available data, assumed zero pH 5.95 7.51 pH estimates are based on probe sampling conducted on Trip 3 for SFCC and Grassy Branch. Slow CBOD (mg/L) 9.49 4.52 Measured CBOD5 from Trip 3 was used to approximate slow Fast CBOD (mg/L) 0 0 CBOD as described in the text. Ammonia N (pgN/L) 110 25 NH3 and NOX data are observed data from Trip 3 at WQ Organic N (pgN/L) 630 705 Site#9 (SFCC) and WQ Site#13 (Grassy Branch). Organic N was calculated as the difference between observed TKN Nitrate+Nitrite N (pgN/L) 5 610 and NH3 data. Organic P (pgP/L) 98 98 Organic P was calculated as the difference between Inorganic P (pgP/L) 92 72 observed TP and PO4 from Trip 3. 3.8 REACH WATER QUALITY PARAMETERS Modeled water quality parameters that can vary by reach include sediment oxygen demand (SOD) rates; prescribed nutrient flux rates from sediment; channel reaeration rates; nutrient hydrolysis and settling rates; phytoplankton growth, respiration, and death rates; and bottom algae coverage, growth, respiration, and death rates. If not otherwise specified for a given reach, water quality parameterization was tabulated using default values and suggested ranges of model inputs. Model inputs related to reaeration, SOD, bottom algae, and phytoplankton can have large influence on average DO and the diurnal range of DO. The DO sondes were used to identify the diurnal variation in DO observed at specific points along Crooked Creek. DO sondes were used to identify the relative impact of bottom algae (surrogate for macrophyte growth) along Crooked Creek based on observed diel DO variation. During the first field sampling trip, DO sondes were placed upstream and downstream of the Crooked Creek#2 discharge and near the crossing of Highway 601. During the second trip, DO sondes TETRA TECH 23 Crooked Creek QUAL2K Model October 15, 2019 were placed at the Highway 601 crossing, at the Brief Road crossing, and at the State Road 1601 crossing. All six sondes experienced a diurnal DO variation between 1.18 and 2.53 mg/I. Diurnal DO fluctuations are due to photosynthetic processes of biota which are light and temperature dependent. The relatively low diurnal fluctuations in DO observed along Crooked Creek suggest that algae play a relatively minor role in the system. Bed coverage of algae was parameterized for the calibration and corroboration models as a forcing function, such that inputs varied between the two models based on observed algal conditions and diel DO variation between the two simulation periods (Table 14). The magnitude of daily minimum and maximum DO are controlled by the streambed coverage of bottom algae as an aggregate term for all macrophyte growth exerting photosynthetic processes within the water column. For the calibration model, reach 1 was parameterized with 25% bottom algae coverage, while all other reaches were set to 50% coverage. Between the field sampling work in August and September, there was additional algal growth observed, such that reach parameterization for bottom algae coverage was increased for the corroboration model run. For this model run, reach 1 was parameterized with 50% bottom algae coverage, while reaches 2, 3, 4, and 6 were set to 75% coverage. Reach 5 was increased further to 95% bottom algae coverage due to the presence of increased algae and multiple DO observation points measured at supersaturation in this reach. Table 14. Model inputs for bottom algae coverage Bottom Algae Coverage Reach Calibration Corroboration 1 25% 50% 2 50% 75% 3 50% 75% 4 50% 75%. 5 50% 95% 6 50% 75% Average instream DO concentrations are sensitive to SOD, which is the consumption of DO at the soil- water interface. SOD is simulated in QUAL2K as both a rate of oxygen consumption as well as a percent coverage of the channel bottom. SOD was not measured along Crooked Creek, so the model was initialized based on the observed range measured in another North Carolina Piedmont-area stream: Rich Fork Creek near High Point (Tetra Tech, 2009b). SOD estimates associated with Rich Fork Creek were also used in the modeling effort associated with Twelve Mile Creek in Union County (Tetra Tech, 2009c). SOD was measured with in situ chambers at a number of locations along Rich Fork Creek, both upstream and downstream of an existing WWTP. The observed range of SOD along Rich Fork Creek was 0.067 — 0.213 g/ft2/d (0.721 —2.293 g/m2/d), with the lowest values generally being recorded upstream of the WWTP discharge. The Crooked Creek model was initialized with instream SOD coverage set to 100% at a rate of 0.067 g/ft2/d (0.721 g/m2/d) for all reaches. This SOD rate was adjusted during calibration adjust simulated DO concentrations to mimic longitudinal profiles. Note that the North Carolina Division of Water Quality has measured SOD across the state periodically and the observed range for the Upper Cape Fear River watershed was approximately 0.4 —2.5 g/m2/d, which provided a constraining range during model calibration. l l TETRA TECH 24 Crooked Creek QUAL2K Model October 15, 2019 Channel reaeration is the natural input of oxygen to a waterbody through the transfer of atmospheric oxygen into the water column at the air-water interface. Rates of reaeration are typically higher for shallow, fast moving streams, and lower for slow, deep streams. Although reaeration was not measured directly in Crooked Creek, anecdotal evidence and observed reaeration from the Rich Fork Creek project was used to confine and inform the Crooked Creek model setup. Rich Fork Creek had observed reaeration rates of 0.32/d in low-velocity pooled areas of the stream, and 1.85/d in free-flowing sections of the stream with observed flows on the order of 27 cfs. The Tsivoglou-Neal reaeration formula was identified as likely appropriate for Crooked Creek as it computes reaeration based on mean water velocity and channel slope and is appropriate for low flow streams where flow ranges 1 — 15 cfs, and the average field-estimated flow along Crooked Creek is about 2.5 cfs (Tsivoglou and Neal, 1976). For model setup, initial assumptions for reach parameters related to nutrient processing, settling rates, and decay were held at model default values and were adjusted during calibration as-needed. TETRA TECH 25 O Crooked Creek QUAL2K Model October 15, 2019 4.0 MODEL CALIBRATION AND CORROBORATION Model calibration involves comparing how well model simulations match observed data. Model calibration is designed to ensure that the model is adequately and appropriately representing the system in order to answer the study questions. The model must be able to provide credible representations of the movement of water, and the DO and BOD interactions within the stream representing steady state conditions. Corroboration is applied using a different time period to confirm that model calibration is robust, provide additional evaluation of model performance, and to guard against over-fitting to the calibration data. The QUAL2K model for Crooked Creek will be calibrated to an average of data collected during the first two sampling trips in August 2016. The corroboration period for the model will be focused on the middle of September during the third and final summer sampling trip. Physical properties related to stream flow and atmospheric inputs may be subject to change during the model corroboration period. The model will be set up for these conditions using available data and calibrated to reproduce observed DO. 4.1 HYDROLOGY CALIBRATION Reach hydraulics were calibrated in order to approximate observed and estimated conditions of flow, depth, and velocity along Crooked Creek during the summer sampling trips. Manning's n was the key calibration parameter that was adjusted to capture site-estimated flow dynamics since the measured cross-sections were considered reasonable enough to approximate channel shapes. The calibrated reach hydraulic inputs were to alter Manning's n to 0.3 for all reaches except Reach 4 (sluggish, pooled beaver dam reach)which had a roughness coefficient of 0.6. Travel time for the full extent of Crooked Creek was estimated by the model to be just over six days, and model results of flow along the mainstem compared to observations may be seen in Figure 13. Along the entire reach, simulated stream velocity ranged from 0.07— 0.16 ft/s (0.02—0.05 m/s) (observed range was 0.13—0.39 ft/s [0.04—0.12 m/s]), and simulated water depth ranged from 0.89—2.13 ft (0.27—0.65 m) (observed range was 0.49—2.10 ft[0.15—0.64 m]). Upstream and downstream streamflow along Crooked Creek were simulated to be 1.06 and 4.24 cfs (0.03 and 0.12 cms) respectively. CTETRA TECH 26 Crooked Creek QUAL2K Model October 15, 2019 SFCC HWY 4.5 confluence 601 • 4.0 CC#2 WWTP • I 3.5 • 3.0 Hemby • Grassy WWTP. v, WWTP • Grassy Branch confluence 2.5 u I • 2.0 j T. 1.5 1.0 0.5 0.0 20 15 10 5 0 Distance from outlet (miles) • Field-Estimated Flow -Simulated Flow:Calibration Model Figure 13. Simulated and site-estimated flows for Crooked Creek model extent (calibration) 4.2 WATER TEMPERATURE CALIBRATION In general, the parameters which control water temperature are channel geometry, meteorological inputs, stream shading, atmospheric heat models, and sediment heat parameters. Initialized parameterization related to sediment thermal properties, stream shading, and heat models captured the observed water temperature data reasonably well. The simulated minimum, maximum, and average water temperature are shown in Figure 14 in comparison with observed water temperature from the YPDRBA in August, longitudinal sampling along the entire extent from sampling trips 1 and 2, and the range of temperatures observed at the sonde locations from trips 1 and 2 as well (Figure 14). Moving from upstream to downstream, it is possible to see that the majority of morning sampling (open circles) fall below the mean simulated water temperature line, while the majority of afternoon sampling (closed circles) fall above the mean simulated water temperature line. The spread of observed temperature data is largely captured by the diel range simulated by the model as seen in the dashed lines below. In general the sonde data which represents the observed range of data over several days at a given point(red vertical lines) are skewed low relative to the longitudinal sampling (points) due to the fact that these sondes were submerged along the stream bed which is anticipated to be cooler and more well-insulated to daily fluctuations than the water closer to the surface. CTETRA TECH 27 Crooked Creek QUAL2K Model October 15, 2019 1--1--1- --2 I---------3---------I--4----I----- -5 I 6 -I 90 • • 70 Beaver HWY 60 Dams 601 50 Hemby CC#2 SFCC Grassy WWTP. 40 WWTP WWTP confluence Grassy Branch confluence 30 A 20 10 0 20 15 10 5 0 Distance from outlet(miles) Simulated Mean Temp ———— Simulated Min/Max Temp Observed Sonde Data • YPORBA Point Data 0 Obs Long Data(AM)Trip I • Obs Long Data(PM)Trip 1 O Obs long data(AM):trip 2 • Obs long data(PM)trip 2 Figure 14. Simulated and observed water temperature along Crooked Creek (calibration) 4.3 WATER QUALITY CALIBRATION The primary focus of water quality calibration was related to DO concentrations along Crooked Creek. The key parameters which control average DO concentrations were identified to be SOD rate and channel reaeration. The magnitude of diel DO variation is controlled by the streambed coverage of bottom algae. Reaeration rates were simulated using the Tsivoglou-Neal model, and were estimated as 0.4—3.3 /d, with an average reaeration rate of 2.3/d. The lowest reaeration rate occurred in the model along the sluggish beaver-dammed Reach 4. SOD rates were used as a calibration parameter, constrained by the range of observed SOD in the Upper Cape Fear River basin from NC DWQ of 0.4—2.5 g/m2/d. Calibrated SOD rates ranged from 1.0—2.2 g/m2/d in the calibrated model, such that reach 1 was assigned 1.0 g/m2/d, while all other reaches were assigned 2.2 g/m2/d to best approximate average instream DO conditions. The simulated minimum, maximum, and average DO are shown in Figure 15 in comparison with observed DO from the YPDRBA in August, longitudinal sampling along the entire extent from sampling trips 1 and 2, and the range of DO observed at the sonde locations from trips 1 and 2 as well. Annotations on the plot below reveal key features along the mainstem such as point source and tributary inflows which may have significant impacts on in-stream DO concentration. From upstream to downstream, it is possible to the see the increase in DO due to the Hemby WWTP discharge, then a decline in DO downstream due to the BOD decay from the effluent. The DO spike at the end of Reach 2 is due to the CC#2 outfall, and the DO decline downstream is smaller downstream relative to downstream of Hemby because of the difference in BOD loading to the stream. The SFCC tributary has low DO, and the DO along the sluggish and dammed Reach 4 causes a precipitous drop in oxygen along that reach. The recovery in DO downstream of the beaver dams and Highway 601 is due to the combined impacts of higher slopes, less in-stream BOD, and the impact of the Grassy Branch WWTP is relatively small as Crooked Creek flows down to Rocky River. The range of daily DO concentrations observed along Crooked Creek is captured reasonably well by the ®TETRA TECH 28 Crooked Creek QUAL2K Model October 15, 2019 calibration model, with DO at the downstream end estimated to be about 6 mg/I at the Rocky River confluence. I--1--I— 2-------I — — 3 I----4 I-- 5 I --- 6------ 112 Hemby CC#2 • SFCC HWY Grassy WWTP, WWTP WWTP confluence 601 Grassy Branch confluence Beaver 10 i I I Dams I • _-------- r"o • • ie----r O • ,,• • 0_ O • `_fin W i • �� `� �'• • .. `,---i--�-} � % • O •O • `i •• r L O % • 0 20 15 10 5 0 Distance from outlet(miles) • YPDRBA Point Data 0 Obs Long Data(AM)Trip 1 • Obg Long Data(PM)Trip 1 o Obs Long Data(AM)Trip 2 • Obs Long Data(PM)Trip 2 Simulated Mean ---- Simulated Min/Max Observed Sonde Data WQS:5.0 mg/I -- DO Saturation Figure 15. Simulated and observed DO along Crooked Creek (calibration) 4.4 MODEL CORROBORATION RESULTS Model corroboration is conducted in order to verify the simulation and parameterization achieved during model calibration reasonably approximates stream conditions during different stream conditions. Although overall stream hydrology is held constant between the calibration and corroboration periods, significant model changes were made for the corroboration regarding the following parameters: model run date, meteorological inputs (air temperature, dew point temperature, and cloud coverage), tributary and headwater chemistry, and point source flow and water chemistry. All other model parameters related to channel geometry, flows, shading, SOD, and reaeration were held constant for the corroboration model run. 4.4.1 Water Temperature Corroboration In general, the water temperature was reasonably well simulated during the model corroboration period. The downstream water temperature from near the end of Reach 5 and into Reach 6 was observed much warmer than the model predicted, but the water temperatures are reasonably well approximated for Reaches 1 through most of Reach 5. The simulated minimum, maximum, and average water temperature are shown in Figure 16 in comparison with observed water temperature from the YPDRBA in September, longitudinal sampling along the entire extent from sampling trip 3, and the range of temperatures observed at the sonde locations from trips 3 as well. CTETRA TECH 29 Crooked Creek QUAL2K Model October 15, 2019 --1------ — 6 — -I 90 _ 80 60 a I Beaver Hwy So lb: Dams 601 40 ar 1- Hemby CC#2 SFCC Grassy WWTP, 30 °_' WW TP WTP confluence Grassy Branch confluence 3 20 10 0 20 15 10 5 0 Distance from outlet(miles) -Simulated Mean Temp ---- Simulated Min/Max Temp Observed Sonde Data • YPDRBA Pant Data 0 Obs Long data(AM) • Obs long data(PM) Figure 16. Simulated and observed water temperature along Crooked Creek (corroboration) 4.4.2 Water Quality Corroboration The simulated minimum, maximum, and average DO during the corroboration period are shown in Figure 17 to reasonably approximate observed DO relative to DO from the YPDRBA in September, longitudinal sampling from sampling trip 3, and the range of DO observed at the sonde locations from trip 3. I--1--I-- 2 I-- — 3 I 4 I s — ---I 6— — — ---1 Hemby CC#2 SFCC HWY Grassy WWTP, 11 WWTP WWTP confluence 601 Grassy Branch confluence Beaver I I 1f Dams I 1 10 -------•-. • 8 a ----r E • i ' o • c ' i I Q- (DIetc --' % • 0 t9 d� ' . v 6 X r 71`k,..........„........„. 0 o• I 16 • I' • , O 2 0 20 15 10 0 Distance from outlet(miles) • YPDRBA Pant Data 0 Obs Long Data(AM) • Obs Long Data(PM) Simulated Mean ---- Simulated Min/Max Observed Sonde Data WQS:5.0 mg/1 DO Saturation Figure 17. Simulated and observed DO along Crooked Creek (corroboration) ( TETRA TECH 30 Crooked Creek QUAL2K Model October 15, 2019 5.0 MODEL SENSITIVITY A series of sensitivity analyses were conducted in order to provide an increased understanding of uncertainty associated with key model parameters. The relative impact of several model parameters were gauged in order to test the model sensitivity to changes in: bottom algae coverage, SOD rate, Manning's n, percent shade, headwater flow rate, and the selected reaeration model (Table 15). Each parameter was tweaked by +25% and -25% with the exception of the reaeration model, for which other formulas were selected in each successive run. Table 15. Crooked Creek QUAL2K model sensitivity test runs Model Run Details Calibration Representative summer conditions for setting up sensitivity analyses Sensitivity 1 Bottom Algae +/-25% Sensitivity 2 SOD Rate +/-25% Sensitivity 3 Manning's n +/-25% Sensitivity 4 Shade +/-25% Sensitivity 5 Headwater Flow +/-25% Sensitivity 6 Reaeration Models: O'Connor-Dobbins, Churchill, Owens-Gibbs, Thackston-Dawson The results from the six sensitivity tests reveal the relative impact each of the tested parameters has on the simulated mean dissolved oxygen concentrations along the extent of the Crooked Creek QUAL2K model. Sensitivity tests 1 and 2 involve a 25% change in bottom algae coverage and SOD rate respectively. These scenarios reveal that the model is more sensitive to SOD rate than bottom algae coverage by impacting mean DO on the order of 16% and 5% respectively (Figure 18). Sensitivity tests 3, 4, and 5 involve a 25% change in Manning's n, shade, and headwater flow respectively. These scenarios reveal the impact to mean DO to be relatively small, on the order of 4-5% for these three tests (Figure 19). Sensitivity test 6 involved testing model sensitivity to reaeration model selection (Figure 20). Of the four reaeration models selected, the impact on mean DO was as follows, from greatest to least: Owens- Gibbs (35%), O'Connor-Dobbins (31%), Churchill (19%), and Thackston-Dawson (11%). Both Owens- Gibbs and O'Connor-Dobbins reaeration models predicted a positive impact on mean DO, while Churchill and Thackston-Dawson reaeration models predicted a negative impact on mean DO relative to the calibration model which used the reaeration model of Tsivoglou-Neal. In general, both Churchill and O'Connor-Dobbins models are only appropriate for streams with depths greater than 1.6 feet(0.5 meters) which is greater than the observed depths in Crooked Creek. The Owens-Gibbs formula overestimates reaeration significantly (similar to O'Connor-Dobbins), likely because Owens-Gibbs assumes high reaeration with low depth, even when velocities are small, but as seen visually along Crooked Creek, low velocities can lead to pooling and stagnation with limited reaeration occurring. The Thackston-Dawson formula responds similarly to the selected model of Tsivoglou-Neal, however it consistently underpredicts instream DO by about 0.5 mg/I. The Tsivoglou-Neal formula remains the best fit to the observed data during both the calibration and corroboration periods (Thackston and Dawson, 2001). The overall results are summarized in Table 16. ®TETRA TECH 31 Crooked Creek QUAL2K Model October 15, 2019 I-1-I 2 I 3 I—4—I —5------ I— --6 -----I 8 Hemby CC#2 SFCC HWY Grassy WWTP, •WWTP iP confluence 601 —— Grassy Branch confluence 1 Beaver Daams -4 . ," .j 1 0 20 15 10 5 0 Distance from outlet (miles) Calibrated Model ---- Sensitivity 1: Bottom Algae ---- Sensitivity 2:SOD Rate Figure 18. Sensitivity test results (runs 1 and 2): bottom algae coverage and SOD rate I-1--I----2-------I— 3 I—4—I -5--------I---------_-6 — - 18 Hemby CC#2 SFCC HWY GrassyWWTP. WWTPP 1 confluence 601 Grassy Branch confluence � Beaver 4 E Dams 6 61 l ,' 4 0 3 0 �N % 2 0 'S 1 v 2 0 20 15 10 5 0 Distance from outlet (miles) Calibrated Model ---- Sensitivity 3: Manning's n ---- Sensitivity 4: Shade Sensitivity 5: Headwater Flow Figure 19. Sensitivity test results (runs 3, 4, and 5): Manning's n, shade, and headwater flow Nit TETRA TECH 32 Crooked Creek QUAL2K Model October 15, 2019 1-1-I 2 I 3---_____I 4-1 5----- I— -6 --_—I 8 Hemby CC#2 SFCC HWY GrassyWWTP. _ WWrP P confluence Beaver 6}- �aS�Y� �itcBalua 7 6 5 "� - - -• -- -�__-- Dams 5 1= i c sy\ ...,......... I I-1-1 7 -. - -- cu to -I 4 -0 1 r - a ' 3 0 41, ` . , 2 r 1 a 1 0 20 15 10 5 0 Distance from outlet (miles) Calibrated Model(Tsivoglou-Neal) ---- Sensitivity 6a: O'Connor Dobbins - - - - Sensitivity 6b:Churchill ---- Sensitivity 6c:Owens Gibbs ---- Sensitivity 6d:Thackson-Dawson 1 Figure 20. Sensitivity test results (run 6): reaeration model selection Table 16. Crooked Creek QUAL2K model sensitivity test run results Average Absolute Average Absolute Model Run Details Difference in Mean DO Relative Percent (mg/I) Difference on Mean DO Calibration Baseline N/A N/A Sensitivity 1 Bottom Algae +/-25% 0.2 5% Sensitivity 2 SOD Rate +/-25% 0.8 16% Sensitivity 3 Manning's n +/-25% 0.2 4% Sensitivity 4 Shade +/-25% 0.2 5% Sensitivity 5 Headwater Flow+/-25% 0.2 4% Sensitivity 6 Reaeration Model Variations 1.1 24% The selection of the reaeration formula can result in the largest single absolute error, however there is reasonably good knowledge that the selected model of Tsivoglou-Neal is the most appropriate choice. The next parameter which the model is quite sensitive to is SOD, which had an average absolute relative percent difference on mean DO of 16%. Since neither reaeration nor SOD were measured directly along Crooked Creek, the interaction between those two parameters are likely the greatest source of uncertainty within the model environment, although estimates for both were established based on reasonable approximations. IA I TETRA TECH 33 Crooked Creek QUAL2K Model October 15, 2019 6.0 REFERENCES Beven, K.J., Gilman, K., and Newson, M. 1979. Flow and flow routing in upland channel networks. Hydro!. Sci. Bull. 24:43-69. Brown, L. C. and T. O. Barnwell, Jr., 1987. The enhanced stream water quality models QUAL2E and QUAL2E-UNCAS: Documentation and User Manual. Tufts University and US EPA, Athens, Georgia. Chapra, S.C., G.J. Pelletier, H. Tao. 2012. QUAL2K: A Modeling Framework for Simulating River and Stream Water Quality, Version 2.12: Documentation and User's Manual. Civil and Environmental Engineering Dept., Tufts University, Medford, MA. Chow, V.T. 1959. Open-channel hydraulics: New York, McGraw-Hill, 680 p. EPA. 1985. Rates, Constants, and Kinetics Formulations in Surface Water Quality Modeling (Second Edition). EPA/600/3-85/040. Leo, WM, RV Thomann, TW Gallaher. 1984. Before and after case studies: comparisons of water quality following municipal treatment plant improvements. EPA 430/9-007. Office of Water, Program Operations, U.S. Environmental Protection Agency, Washington, DC. National Service Center for Environmental Publications (NCASI). 1985. Computer program documentation for the enhanced stream water quality model QUAL2E. EPA/600/3-85. North Carolina Department of Natural Resources (NC DENR). 2016. 2016 303(d) Listing Methodology. Tetra Tech. 2009a. Loading Simulation Program in C++ (LSPC)Version 3.1 User's Manual. Fairfax, VA. Tetra Tech. 2009b. Hydrology and Hydraulic Modeling Report for Rich Fork Creek, NC. Prepared for City of High Point and Hazen & Sawyer. Prepared by Tetra Tech. Tetra Tech. 2012a. Goose and Crooked Creek Local Watershed Plan (LWP). Prepared for North Carolina Ecosystem Enhancement Program (NCEEP). Prepared by Tetra Tech. Tetra Tech. 2012b. Goose Creek and Crooked Creek Watersheds: Model Development and Calibration (LSPC Model). Prepared for Centralina Council of Governments and North Carolina Division of Water Quality. Prepared by Tetra Tech. Tetra Tech. 2012c. QUAL2 Model Update for Twelve Mile Creek below the Union County WWTP. Prepared for Union County Public Works Department and Hazen & Sawyer. Prepared by Tetra Tech. Thackston, E.L., and J.W. Dawson. 2001. Recalibration of a reaeration equation. Journal of Environmental Engineering, ASCE, 127(4), 317-321. Tsivoglou, E. C., L.A. Neal. 1976. Tracer Measurement of Reaeration. III. Predicting the Reaeration Capacity of Inland Streams. Journal of the Water Pollution Control Federation, 48(12):2669-2689. United States Army Corps of Engineers (USACE). 2016. HEC-RAS River Analysis System User's Manual. Davis, California. Weaver, J.C., and J.M. Fine. 2003. Low-Flow Characteristics and Profiles for the Rocky River in the Yadkin-Pee Dee River Basin, North Carolina, through 2002. USGS Water-Resources Investigations Report 03-4147. f1TETRA TECH 34 Crooked Creek QUAL2K Model October 15, 2019 ' APPENDIX A: PERMITTED POINT SOURCE DATA Included here are the treated effluent flow and water quality data associated with the permitted point sources in the Crooked Creek watershed for August and September 2016 (Table A-1, Table A-2, and Table A-3). Note that parameters such as chemical oxygen demand (COD), TN, TP, and hardness were measured only once per month at some sites. Also reported by Carolina Water Services, Inc. are instream water quality conditions immediately upstream and downstream of the Hemby Acres WWTP which were used for headwater condition parameterization and instream calibration (Table A-4). Table A-1. DMR data from August and September 2016: Crooked Creek#2 WWTP (NC0069841) Flow Temp BOD5 NH3 TSS DO COD TN TP Hardness Alkalinity Date (MOD) (°F) pH (mg/I) (mg/I) (mg/I) (mg/I) (mg/I) (mg/I) (mg/I) (mg/I) (mg/I) 8/1/16 0.71 80.4 7.5 <2 <.1 <2.5 7.8 8/2/16 0.86 78.8 7.3 <2 0.91 <2.5 7.8 8/3/16 0.85 78.8 7.4 <2 0.92 <2.5 7.6 88 8/4/16 0.79 78.8 7.4 <2 1.0 <2.5 7.7 8/5/16 0.80 77.4 7.3 <2 0.87 <2.6 5.5 8/6/16 0.92 8/7/16 0.81 8/8/16 0.89 79.7 7.3 <2 3.3 <2.5 7.6 8/9/16 0.95 79.3 7.3 <2 4.7 <2.5 7.6 8/10/16 0.91 80.2 7.2 <2 3.5 <2.6 7.4 33 6.4 3.3 74 91 8/11/16 1.11 80.2 7.4 2.2 7.6 8/12/16 0.87 82.4 7.2 6.8 8/13/16 0.26 8/14/16 0.75 8/15/16 0.79 82.0 7.5 2.9 <.1 2.5 7.7 8/16/16 0.82 81.5 7.6 <2 <.1 <2.5 7.9 8/17/16 0.80 81.1 7.5 <2 <.1 <2.5 8.0 85 8/18/16 0.85 80.8 7.3 7.8 8/19/16 0.95 80.6 7.0 7.4 8/20/16 0.89 8/21/16 0.84 8/22/16 0.80 80.6 7.3 <2 <.1 <2.5 7.9 8/23/16 0.82 78.8 7.3 <2 <.1 <2.5 7.9 8/24/16 0.76 77.9 7.3 <2 <.1 <2.5 8.0 65 8/25/16 0.77 77.5 7.3 <2 <.1 <2.5 8.1 8/26/16 0.81 80.6 6.7 <2.5 7.2 OTETRA TECH 35 Crooked Creek QUAL2K Model October 15, 2019 Flow Temp BOD5 NH3 TSS DO COD TN TP Hardness Alkalinity Date (MGD) (°F) pH (mg/I) (mg/I) (mg/I) (mg/I) (mg/I) (mg/I) (mg/I) (mg/I) (mgll) 8/27/16 0.81 8/28/16 0.94 8/29/16 0.90 79.0 7.1 2.5 <.1 4.3 80 8/30/16 0.81 78.8 7.1 <2 <.1 2.7 8.0 8/31/16 0.77 80.1 7.1 <2 <.1 <2.6 7.9 38 9/1/16 0.78 78.4 7.2 <2 <.1 <2.5 8.0 9/2/16 0.86 80.6 6.8 7.8 9/3/16 1.85 9/4/16 0.91 9/5/16 0.75 77.0 6.9 7.3 9/6/16 0.79 76.1 7.3 <2 <.1 <2.5 8.2 9/7/16 0.89 76.6 7.2 <2 <.1 3.9 8.0 9/8/16 0.81 77.4 7.2 2.7 <.1 6.5 7.9 27 30.35 4.8 150 52 9/9/16 0.78 77.7 7.2 5.2 <.1 10.4 8.0 9/10/16 0.78 9/11/16 0.78 9/12/16 0.80 77.7 7.1 6.8 0.11 19 8.0 9/13/16 0.89 76.8 7.1 2.4 <.1 8.4 8.1 9/14/16 0.79 77.5 7.0 2.0 <.1 7.6 7.9 34 9/15/16 0.79 77.5 7.0 8.0 9/16/16 0.78 78.8 6.4 2.6 <.1 6.6 7.9 9/17/16 0.76 9/18/16 0.80 9/19/16 0.81 78.6 6.4 <2 0.11 4.6 7.9 9/20/16 0.81 77.5 6.8 <2 <.1 3.0 8.0 9/21/16 0.82 75.4 7.2 <2 <.1 <2.6 8.2 27 9/22/16 0.88 75.2 7.2 <2 <.1 <2.6 8.3 9/23/16 1.07 75.9 6.4 7.9 9/24/16 0.89 9/25/16 0.86 9/26/16 0.96 76.6 7.4 <2 <.1 <2.6 8.2 9/27/16 0.89 75.9 7.6 8.3 9/28/16 0.95 76.8 7.3 3 <.1 <2.5 8.1 9/29/16 0.84 76.1 7.3 <2 <.1 <2.5 8.2 9/30/16 0.87 77.0 7.3 <2 <.1 <2.5 7.7 TETRA TECH 36 Crooked Creek QUAL2K Model October 15, 2019 Table A-2. DMR data from August and September 2016: Grassy Branch WVVTP (NC0085812) Flow Temp BOD5 NH3 TSS DO COD Alkalinity Date (MGD) (°F) pH (mg/I) (mg/I) (mg/I) (mg/I) (mg/I) (mg/I) 8/1/16 0.01 80.6 7.1 8/2/16 0.05 75.2 7.3 2.4 0.32 2.7 7.75 30 59 8/3/16 0.03 75.2 7.1 8/4/16 0.03 77.0 7.5 8/5/16 0.02 77.0 7.5 8/6/16 0.32 8/7/16 0.02 8/8/16 0.07 77.0 7.8 8/9/16 0.11 77.0 7.8 8/10/16 0.04 78.8 7.8 8/11/16 0.03 78.8 7.2 <2 <.1 <2.6 7.95 87 8/12/16 0.03 78.8 7.7 8/13/16 0.18 8/14/16 0.02 8/15/16 0.02 82.4 7.7 8/16/16 0.02 80.6 7.6 <2 <.1 <2.6 7.04 96 8/17/16 0.02 80.6 7.2 8/18/16 0.02 82.4 7.3 8/19/16 0.04 78.8 7.5 8/20/16 0.03 8/21/16 0.02 8/22/16 0.02 78.8 7.2 8/23/16 0.02 77.0 7.0 <2 <.1 2.6 8.25 131 8/24/16 0.02 77.0 7.0 8/25/16 0.03 77.0 7.0 2 <.1 <2.5 7.3 120 8/26/16 0.03 78.8 7.3 8/27/16 0.02 8/28/16 0.03 8/29/16 0.03 78.8 7.0 TETRA TECH 37 Crooked Creek QUAL2K Model October 15, 2019 Date Flow Temp BOD5 NH3 TSS DO COD Alkalinity (MGD) (°F) pH (mg/I) (mg/I) (mg/I) (mg/I) (mg/I) (mg/I) 8/30/16 0.03 77.0 6.9 3.4 3.3 5.6 7.88 8/31/16 0.03 77.0 6.6 9/1/16 0.04 78.8 6.9 <2 1.2 <2.5 7.52 59 9/2/16 0.03 78.8 7.1 9/3/16 0.10 9/4/16 0.03 9/5/16 0.02 77.0 7.4 9/6/16 0.04 78.8 7.4 9/7/16 0.03 77.0 6.8 <2 <.1 <2.6 7.98 74 9/8/16 0.04 75.2 6.7 <2 <.1 <2.5 7.38 67 9/9/16 0.03 77.0 6.9 9/10/16 0.03 9/11/16 0.02 9/12/16 0.02 78.8 7.0 9/13/16 0.03 77.0 6.3 <2 0.34 <2.5 7.19 19 38 9/14/16 0.03 77.0 6.6 <2 0.46 <2.5 7.16 62 9/15/16 0.04 75.2 6.8 9/16/16 0.04 77.0 7.3 9/17/16 0.03 9/18/16 0.02 9/19/16 0.02 77.0 7.7 9/20/16 0.04 75.2 7.6 9/21/16 0.03 73.4 7.1 <2 <.1 <2.5 8.35 164 9/22/16 0.04 73.4 7.1 <2 <.1 <2.6 7.49 176 9/23/16 0.05 75.2 7.0 9/24/16 0.05 9/25/16 0.02 9/26/16 0.04 77.0 7.7 9/27/16 0.05 73.4 6.7 9/28/16 0.10 77.5 7.8 CTETRA TECH 38 Crooked Creek QUAL2K Model October 15, 2019 Flow Temp BOD5 NH3 TSS DO COD Alkalinity Date (MGD) (°F) pH (mg/I) (mg/I) (mg/I) (mg/I) (mg/I) (mg/I) 9/29/16 0.03 74.5 7.2 <2 <.1 <2.5 8.34 -_ 9/30/16 0.04 74.5 7.3 <2 <.1 <2.6 7.35 -_ Table A-3. DMR data from August and September 2016: Hemby Acres WWTP (NC0035041) Flow Temp BOD5 NH3 TSS DO Date (MGD) (°F) pH (mg/I) (mg/I) (mg/I) (mg/I) 8/1/16 0.06 80.4 7.0 6.72 8/2/16 0.08 8/3/16 0.09 79.0 7.3 2.3 <0.1 <2.5 7.38 8/4/16 0.09 8/5/16 0.08 ' 8/6/16 0.13 8/7/16 0.08 8/8/16 0.07 8/9/16 0.10 8/10/16 0.10 79.5 8.0 8/11/16 0.10 78.6 7.6 4.6 <0.1 <2.5 6.73 8/12/16 0.09 8/13/16 0.10 8/14/16 0.10 8/15/16 0.06 8/16/16 0.09 76.8 6.8 5.84 8/17/16 0.09 8/18/16 0.08 80.2 7.7 <2 <0.1 <2.5 6.5 8/19/16 0.10 8/20/16 0.08 8/21/16 0.09 8/22/16 0.12 8/23/16 0.07 76.3 7.8 5.31 8/24/16 0.09 ®TETRA TECH 39 Crooked Creek QUAL2K Model October 15, 2019 Date Flow Temp BOD5 NH3 TSS DO (MGD) (°F) pH (mg/I) (mg/I) (mg/I) (mg/I) 8/25/16 0.07 75.6 7.3 <2 <0.1 <2.5 6.65 8/26/16 0.09 8/27/16 0.14 8/28/16 0.06 8/29/16 0.09 8/30/16 0.09 75.6 8.1 12 <0.1 <2.5 6.62 8/31/16 0.11 9/1/16 0.07 76.8 7.6 6.2 9/2/16 0.10 9/3/16 0.18 9/4/16 0.08 9/5/16 0.09 9/6/16 0.06 73.9 7.0 6.55 9/7/16 0.09 9/8/16 0.08 74.5 7.0 11 <0.1 <2.5 6.1 9/9/16 0.08 9/10/16 0.11 9/11/16 0.08 75.2 7.2 7.01 9/12/16 0.07 76.1 8.2 4.9 <0.1 <2.5 7.21 9/13/16 0.09 9/14/16 0.10 9/15/16 0.07 9/16/16 0.09 9/17/16 0.09 9/18/16 0.08 9/19/16 0.11 9/20/16 0.09 75.9 7.4 6.61 9/21/16 0.08 9/22/16 0.10 76.6 7.3 3.2 <0.1 <2.5 6.87 9/23/16 0.10 TETRA TECH 40 Crooked Creek QUAL2K Model October 15, 2019 Flow Temp BOD5 NH3 TSS DO Date (MGD) (°F) pH (mg/I) (mg/I) (mg/I) (mg/I) 9/24/16 0.08 9/25/16 0.08 9/26/16 0.08 9/27/16 0.04 75.7 7.1 7.33 9/28/16 0.20 75.4 7.2 4.5 <0.1 <2.5 7.12 9/29/16 0.07 9/30/16 0.09 Table A-4. Instream DMR water quality data upstream and downstream of Hemby Acres VWVTP, August and September 2016 Temperature (°F) Dissolved Oxygen (mg/I) Date Upstream Downstream Upstream Downstream 8/3/16 74.8 75.4 4.72 5.03 8/11/16 73.8 75.2 4.57 5.03 8/18/16 76.3 76.8 4.43 4.96 8/25/16 73.6 75.0 3.33 4.01 8/30/16 73.4 75.0 4.32 4.91 9/8/16 71.6 73.2 4.01 4.59 9/12/16 71.8 73.2 3.63 4.97 9/22/16 73.9 76.3 3.65 4.01 9/28/16 68.2 69.8 4.22 4.98 ®TETRA TECH 41 Crooked Creek QUAL2K Model October 15, 2019 APPENDIX B: YPDRBA COALITION DATA Water quality sampling conducted by the Yadkin Pee Dee River Basin Association (Coalition) during August and September of 2016 may be relevant to use for model calibration and corroboration (Table B-1). Table B-1. Coalition water quality data of-interest from August and September 2016 Sampling Site Parameter Date* Q8386000 (NFCC Q8386200 (NFCC Q8388000 (CC at SR 1520) at SR1514) at NC 218) 8/9/2016 77.2 77.2 78.8 Water Temperature (°F) 8/30/2016 76.6 76.8 76.5 9/13/2016 73.6 73.8 74.8 8/9/2016 5.8 5.8 6.3 Dissolved Oxygen (mg/I) 8/30/2016 5.7 5.8 6.4 9/13/2016 5.5 5.7 6.5 8/9/2016 6.6 6.6 6.8 pH (s.u.) 8/30/2016 6.6 6.6 6.9 9/13/2016 6.6 6.6 6.8 8/9/2016 263 289 162 Conductivity (umhos/cm) 8/30/2016 393 372 219 9/13/2016 248 229 179 8/9/2016 310 270 166 Fecal Coliform (#/100m1) 9/13/2016 300 250 162 8/9/2016 No Data No Data 9.1 Suspended Residue (mg/I) 9/13/2016 No Data No Data 20 8/9/2016 16 20 16 Turbidity (NTU) 9/13/2016 21 11 11 8/9/2016 No Data No Data 0.1 Ammonia as N (mg/I) 9/13/2016 No Data No Data 0.08 TKN as N (mg/I) 9/13/2016 No Data No Data 0.8 8/9/2016 No Data No Data 1.74 NOX as N (mg/I) 9/13/2016 No Data No Data 2.49 TP (mg/I) 9/13/2016 No Data No Data 0.76 *Note: some samples were taken 1 day before or after the reported date listed in this table 42 Fl.)TETRA TECH Crooked Creek QUAL2K Model October 15, 2019 APPENDIX C: TETRA TECH 2016 SAMPLING DATA C.1 STREAM HYDROLOGY MEASUREMENTS Twenty cross-sections were measured during the 2016 summer sampling effort(Table C-1). Table C-1. Measured reach properties, summer 2016 Distance from Sample Point Width (ft) Velocity Maximum Site-Estimated Headwaters (km) ID (ftls) Depth (ft) Flow (cfs) 2.21 8 16 No Data 1.1 No Data 2.92 13 13 0.30 0.5 1.54 5.15 26 18 0.15 0.9 1.63 5.58 33 10 No Data 0.6 No Data 5.93 3 No Data No Data No Data No Data 6.20 35 19 0.22 2.1 6.25 10.43 61 14 0.26 1.1 2.23 12.45 75 17 0.30 0.8 2.83 14.63 87 23 0.40 0.5 3.29 15.68 1 27 No Data 0.2 No Data 18.71 252 16.5 0.28 0.8 2.42 21.26 117 41.5 No Data 0.6 No Data 22.09 138 24 0.33 1.0 3.61 22.90 118 40.6 No Data 1.6 No Data 23.33 119 38 No Data 1.1 No Data 25.28 160 38.5 0.18 1.0 4.11 26.34 120 28.5 No Data 1.1 No Data 27.59 121 26.5 No Data 1.2 No Data 27.79 122 30 No Data 1.8 No Data 29.23 182 35 0.03 1.1 0.84 •-1 43 TETRA TECH Crooked Creek QUAL2K Model October 15, 2019 C.2 NUTRIENT SAMPLING Grab samples were analyzed for water quality constituents along Crooked Creek during each sampling effort. Fifteen samples were taken from the main stem, tributaries, and wastewater treatment plant discharge sites during each sampling trip (Figure C-1). Water quality analyses were conducted by Pace Analytical laboratory for the following parameters: 5-day biochemical oxygen demand (BOD5), 5-day carbonaceous biochemical oxygen demand (CBOD5), ammonia (NH3), nitrate and nitrite (NO2+NO3), phosphate (PO4), total Kjeldahl nitrogen (TKN), total nitrogen (TN), and total phosphorus (TP). For a number of laboratory samples, the measured parameter was found to be below the level of detection (LOD). The laboratory equipment did produce a numerical result below the LOD which has been included and flagged as such. Although these results are below the LOD, the numbers seem reasonable and may be relevant to include in modeling efforts with an increased level of uncertainty associated with the exact concentrations. The results from all grab samples have been compiled by sampling location, parameter, and trip (Table C-1, Table C-2, and Table C-3). 13 14 is 12 .111 , 11 All. .., it 10 t,, 1 2 3 9 * ar if 5 6 7 8 „.;,., 7471/ -'..-.0 Oa 00, 410111111611 .... A ....,,.. 'Note.Sde 9 was sampled further upstream 1 on South Fork Crooked Creek during the ilikilliVit: , ,„ .. 1,. second and third sampling efforts Legend Grab Sample Site ! • WWTP Discharge Crooked Creek Watershed N A o 0.5 , 2 - NHD HiRes Flowilne [lb)TETRA TECH Water Quality Grab Samples vaiometers M o o s z ® Watershed Boundary .w ox,.:n le NY.* Miles r Figure C-1. Water quality grab sample locations ( )TETRA TECH 44 Crooked Creek QUAL2K Model October 15, 2019 Table C-2. BOD/CBOD results (units mg/I) BOD5 CBOD5 ID Location Note 1 2 3 1 2 3 1 US of Hemby discharge 1.40* 1.20* 4.10 1.10* 1.20* 0.60* 2 Hemby VVWTP discharge 0.70* 2.60 1.40* 0.70* 3.20 2.10 3 Indian Trail Fairview Rd 1.30* 2.00* 1.50* 0.80* 1.60* 1.60* 4 Crooked Creek#2 discharge 1.50* 0.70* 2.20 0.80* 0.50* 1.50* 5 US of CC#2 WWTP discharge 1.50* 1.30* 1.40* 1.00* 1.20* 1.90* 6 Old Farm Bridge crossing 1.60* 1.00* 0.90* 1.40* 0.60* 0.30* 7 DS of Rocky River Rd 1.50* 0.50* 1.20* 1.00* 0.95* 0.50* 8 Ridge Road crossing 1.50* 0.60* 3.50 0.80* 0.90* 0.90* 9 SF Crooked Creek 1.40* 2.00 0.80* 0.90* 1.20* 2.10 10 DS of debris dams 1.40* 0.70* 0.90* 1.10* 0.90* 0.30* 11 Brief Rd crossing 1.40* 1.30* 0.70* 0.90* 1.20* 0.50* 12 Grassy Branch WWTP discharge 0.70* 1.10* 1.70* 0.20* 1.10* 0.10* 13 Grassy Branch Tributary 9.00 8.10 0.90* 3.00 7.50 1.10* 14 Hwy 218 crossing 1.10* 0.60* 0.90* 0.00* 0.80* 0.60* 15 US of Brief Rd 1.00* 0.70* 1.10* 0.50* 0.70* 0.40* *reflects the numerical result reported from lab analysis although result is below reporting limit. Report limit for BOD5: 2.0 mg/I, CBOD5: 2.0 mg/I ®TETRA TECH 45 Crooked Creek QUAL2K Model October 15, 2019 Table C-3. Nitrogen species results (units mg/I) NH3-N NO2+NO3-N TKN TN ID Location Note 1 2 3 1 2 3 1 2 3 1 2 3 1 US of 0.08* 0.03* 0.02* 0.34 0.22 0.08 0.46* 0.94 0.73 0.81 1.20 0.80 Hemby discharge 2 Hemby 0.02* 0.05* 0.02* 33.70 42.30 25.10 0.98 0.00* 1.10 34.70 42.30 26.30 WWTP discharge 3 Indian Trail 0.00* 0.07* 0.08* 6.50 3.20 5.40 0.79 0.54 0.98 7.30 3.70 6.30 Fairview Rd 4 Crooked 0.00* 0.02* 0.00* 24.00 32.90 33.90 1.20 1.10 1.90 25.10 33.90 35.80 Creek#2 discharge 5 US of CC#2 0.09* 0.08* 0.15 2.30 0.51 0.70 0.53 0.69 1.40 2.80 1.20 2.10 WWTP discharge 6 Old Farm 0.12 0.05* 0.04* 10.80 20.50 28.90 1.00 1.30 1.50 11.80 21.80 30.50 Bridge crossing 7 DS of Rocky 0.02* 0.05* 0.04* 11.70 23.30 24.10 1.20 0.63 1.50 12.90 23.90 25.50 River Rd 8 Ridge Road 0.03* 0.05* 0.03* 10.30 16.40 33.20 1.20 1.10 1.10 11.40 17.40 34.30 crossing 9 SF Crooked 0.07* 0.93 0.11 5.60 0.13 0.00* 1.50 1.60 0.74 7.10 1.70 0.74 Creek 10 DS of debris 0.08* 0.07* 0.13 0.46 1.50 8.40 0.92 0.56 1.20 1.40 2.00 9.60 dams 11 Brief Rd 0.00* 0.02* 0.01* 0.34 2.90 0.67 0.67 0.73 0.75 1.00 3.70 1.40 crossing 12 Grassy 0.01* 0.44 0.03* 34.00 44.00 53.30 1.30 0.84 0.00* 35.30 44.80 53.30 Branch WWTP discharge 13 Grassy 0.00* 0.02* 0.02* 1.50 1.70 0.61 0.79 0.25* 0.73 2.30 1.90 1.30 Branch Tributary 14 Hwy 218 0.02* 0.07* 0.02* 1.20 3.80 2.50 0.44* 0.70 0.56 1.60 4.50 3.10 crossing 15 US of Brief 0.01* 0.03* 0.00* 0.55 13.80 0.89 0.47* 0.72 0.46* 1.00 14.50 1.30 Rd `reflects non-detect, numerical result reported Reporting limit for NH3-N: 0.10 mg/I, NO2+NO3-N: 0.020 mg/I,TKN: 0.50 mg/I, TN: 0.12 mg/I. ®TETRA TECH 46 Crooked Creek QUAL2K Model October 15, 2019 Table C-4. Phosphorus species results (units mg/I) PO4-P TP ID Location Note 1 2 3 1 2 3 1 US of Hemby discharge 0.13 0.10 0.05 0.06 0.16 0.12 2 Hemby VWVTP discharge 1.80 4.80 4.00 3.20 5.00 5.60 3 Indian Trail Fairview Rd 0.54 2.10 0.50 0.47 0.47 0.57 4 Crooked Creek#2 discharge 2.90 4.60 4.80 2.50 4.80 6.10 5 US of CC#2 VVWTP discharge 0.31 1.10 0.16 0.24 0.23 0.36 6 Old Farm Bridge crossing 1.20 2.90 4.10 1.20 2.70 4.50 7 DS of Rocky River Rd 1.30 ' 3.30 3.60 1.20 3.00 3.90 8 Ridge Road crossing 0.32 2.40 3.60 1.10 2.20 4.00 9 SF Crooked Creek 0.34 0.15 0.09 1.10 0.15 0.19 10 DS of debris dams 0.23 2.10 1.10 0.84 0.53 1.10 11 Brief Rd crossing 0.86 2.70 0.43 0.72 0.66 0.65 12 Grassy Branch VWVTP discharge 0.30 3.40 4.50 2.70 3.30 4.70 13 Grassy Branch Tributary 0.20 0.26 0.07 0.19 0.12 0.17 14 Hwy 218 crossing 0.16 1.00 0.74 0.75 0.86 0.80 15 US of Brief Rd 0.14 1.90 0.75 0.66 1.60 0.61 Reporting limit for PO4-P: 0.050 mg/I, TP: 0.050 mg/I. ' TETRA TECH 47 Crooked Creek QUAL2K Model October 15. 2019 C.3 LONGITUDINAL DISSOLVED OXYGEN Dissolved Oxygen was monitored using a hand-held probe every several hundred meters along the extent of Crooked Creek on each sampling effort to some degree. The results of the raw DO readings at each location sampled from each trip are seen below (Figure C-2. Figure C-3. Figure C-4. Table C-5. Table C-6, Table C-7). Note that these results have not been temperature-corrected. Frequently sampled alongside dissolved oxygen concentration were: pH, dissolved oxygen saturation, water temperature, turbidity, and specific conductivity. / • _.., 4 .., „._.2_ . _ , . .. ,,,, . it:71, Itiot. • ..1. 40 , .... .._ Legend , WWTP Discharge \ ® Large Beaver Dam NHD HiRes Rowline nWatershed Boundary DO (mg/L) 4.0-5.0 Crooked Creek Watershed N 0 05 1 2 • >5.0 7rtTETRA TECH Longitudinal DO Sampling(8/15-8/19) A ...Kilometers I 4,IOW eY ti Yo.Cana,002 3200 Fm. 0 0 5 1 z No Data wo, ..e aai.ian+n w+w.nw. Miles Figure C-2. instream longitudinal dissolved oxygen measurements (8/15/16-8/19/16) TETRA TECH 48 Crooked Creek QUAL2K Model October 15, 2019 ,._A ,?4. ilt .„ , , .„- ..... ,. , ... y \,,-- °" °""'"' Legend 1 • WWTP Discharge A Large Beaver Dam NHD HiRes Flowline Watershed Boundary DO (mg/L) s° 4.0-5.0 Crooked Creek Watershed N 0 0 5 1 2 • >5.0 Et TETRATECH Longitudinal DOnorth Sampling(8/31-9/2) A °Kilometers Comm..1�s °� 0 05 , 2 No Data A.:r .m,xe 7o, ol Miles Figure C-3. Instream longitudinal dissolved oxygen measurements (8/31/16-9/2/16) [It TETRA TECH 49 Crooked Creek QUAL2K Model October 15. 2019 t . ---4 eA ' .1 .00 Lae P. aw Legend �--- . WWTP Discharge ® Large Beaver Dam `°, NHD HiRes Flowline QWatershed Boundary DO (mg/L) .\ • <4.0 4.0-5.0 Crooked Creek Watershed N 0 05 1 2 • >5.0 (E TETRA TECH Longitudinal DO Sampling(9/13-9/16) A — Knometers ll 0 0.5 1 z No Data 1.P.C....w1i-x1e H�na.. Miles Figure C-4. Instream longitudinal dissolved oxygen measurements (9/13/16-9/16/16) It)TETRA TECH 50 Crooked Creek QUAL2K Model October 15, 2019 Table C-5. Longitudinal data from trip 1 (August 15-19, 2016) ID Latitude(N) Longitude (W) Date Time pH DO(mg/I) DO(%Sat) Temp(°F) 1 35.1074 80.63715 8/15 17:48 6.29 No Data 58.9 79.2 2 35.10429 80.63447 8/15 18:18 6.84 No Data 68.8 80.1 4 35.10346 80.62941 8/15 18:30 6.91 No Data 62 79.5 5 35.10547 80.62941 8/16 8:02 6.95 3.18 39.2 78.3 6 35.10545 80.62855 8/16 8:22 6.99 4.13 51.2 79.0 8 35.10617 80.6272 8/16 8:40 7.14 4.03 49.1 78.3 10 35.10659 80.62418 8/16 9:14 7.13 5.07 61.6 77.5 1 13 35.10786 80.62229 8/16 9:34 7.1 4.67 55.9 77.4 15 35.10893 80.62077 8/16 10:06 7.18 4.79 58.3 77.4 18 35.109 80.61813 8/16 10:40 7.21 4.68 57.5 77.7 19 35.1076 80.61507 8/16 11:01 7.04 2.97 36.3 78.1 20 35.10626 80.6144 8/16 11:13 7.12 3.65 44.7 78.1 21 35.1044 80.61324 8/16 11:27 7.22 3.15 38.8 78.1 22 35.10303 80.61198 8/16 11:41 7.09 4.5 55.1 78.1 24 35.10164 80.61172 8/16 11:51 7.12 4.53 55.3 77.9 25 35.10003 80.6083 8/16 12:11 7.09 4.78 58.4 77.9 26 35.09868 80.60705 8/16 12:25 7.17 4.43 54.2 77.9 28 35.0975 80.60536 8/16 12:58 7.12 3.13 38.4 78.3 30 35.09652 80.60519 8/16 13:05 7.1 3.24 39.9 78.8 31 35.09602 80.60497 8/16 1:13 6.81 2.29 29.4 80.8 32 35.0961 80.60487 8/16 1:19 7.24 5.22 64.5 79.3 33 35.09645 80.6043 8/16 13:32 7.09 5.11 63.4 79.5 34 35.09502 80.60084 8/16 14:02 7.02 2.62 32.3 79.2 35 35.09652 80.59822 8/16 14:38 7.38 5.2 66.2 81.5 ICI TETRA TECH 51 Crooked Creek QUAL2K Model October 15, 2019 ID Latitude(N) Longitude(W) Date Time pH DO(mg/I) DO(%Sat) Temp (°F) 36 35.09743 80.59677 8/16 15:16 7.31 5.13 64.9 81.7 38 35.09833 80.59464 8/16 15:33 7.37 3.89 49.1 81.1 39 35.0989 80.59364 8/16 15:47 7.28 3.25 39.9 80.8 41 35.09908 80.59235 8/16 16:00 7.27 3.57 44.9 80.8 43 35.10103 80.58817 8/16 16:22 8.66 11.64 152.3 85.3 45 35.10244 80.58469 8/16 16:48 7.93 7.2 90.4 83.3 46 35.10362 80.58096 8/17 8:28 7.29 3.85 48.2 79.9 48 35.10303 80.57883 8/17 8:43 7.48 5.53 69.8 80.2 50 35.10158 80.57745 8/17 9:00 7.47 4.48 56.8 80.1 52 35.10235 80.57418 8/17 9:14 7.44 4.42 55.1 79.7 53 35.10264 80.57316 8/17 9:32 7.38 4.34 54.3 79.5 1 54 35.10268 80.57128 8/17 9:53 7.28 4.44 55.3 79.7 56 35.10316 80.56911 8/17 10:15 7.31 2.39 29.9 79.7 58 35.10502 80.56769 8/17 10:36 7.31 4.64 58.5 80.8 60 35.10611 80.56563 8/17 10:54 7.38 3.77 46.1 79.9 61 35.10641 80.56356 8/17 11:32 7.33 3.91 48.8 79.9 62 35.1075 80.56329 8/17 11:48 7.4 4.01 50.2 79.7 63 35.10954 80.56135 8/17 12:13 7.28 5.28 65 78.6 64 35.11013 80.55966 8/17 12:28 7.41 5.13 64.4 80.4 65 35.1108 80.55741 8/17 12:42 7.77 8.08 102.9 82.6 66 35.11146 80.55566 8/17 12:55 7.63 5.03 63 80.4 67 35.11067 80.55408 8/17 13:10 7.4 4.46 56.8 81.7 69 35.11141 80.55309 8/17 13:27 7.36 2.99 37.8 81.1 71 35.11172 80.5519 8/17 13:41 7.33 3 38 81.3 72 35.11196 80.55107 8/17 13:56 7.34 3.21 40.3 80.8 CTETRA TECH 52 Crooked Creek QUAL2K Model October 15, 2019 ID Latitude(N) Longitude(W) Date Time pH DO(mg/I) DO(%Sat) Temp (°F) 74 35.11223 80.54912 8/17 14:23 7.34 3.52 45 81.5 76 35.11278 80.54745 8/17 14:57 7.33 3.9 49.5 81.7 77 35.11274 80.54661 8/17 15:08 7.35 2.47 31.5 81.9 78 35.11441 80.54568 8/17 15:35 7.16 1.22 15.1 79.5 79 35.11661 80.54506 8/17 15:55 7.14 1.1 13.7 79.7 80 35.11855 80.54276 8/17 16:16 7.11 1.9 23.3 80.8 82 35.14477 80.4716 8/18 8:34 7.15 4.27 51.9 77.4 83 35.1331 80.48961 8/18 8:49 7.26 5.3 54.7 77.9 84 35.13116 80.49425 8/18 9:07 7.34 3.7 44.8 76.6 85 35.13099 80.49411 8/18 9:14 6.68 2.78 32.9 74.5 86 35.12245 80.54194 8/18 10:59 6.95 0.82 10.2 78.4 87 35.12229 80.54069 8/18 11:21 7.04 4.43 54.5 79.0 90 35.12278 80.53825 8/18 11:38 7.12 3.64 43.2 78.1 92 35.12492 80.53868 8/18 11:57 7.07 2.78 34 77.7 94 35.12695 80.53902 8/18 12:13 7.06 3.13 38.7 78.3 95 35.12815 80.53928 8/18 12:23 7.02 2.87 35.2 78.1 96 35.12911 80.53567 8/18 12:38 7.05 3.02 37.3 78.6 97 35.12745 80.53224 8/18 13:02 7.05 2.69 32.9 78.8 99 35.12849 80.53107 8/18 13:14 7.2 5.12 63.7 79.7 101 35.12836 80.52878 8/18 13:48 7.3 4.86 60.3 79.5 102 35.12998 80.5269 8/18 14:00 7.35 6.7 83.9 80.4 105 35.13273 80.52562 8/18 14:21 7.48 5.1 63.7 79.9 106 35.1348 80.5248 8/18 14:42 7.29 4.51 56.6 80.2 108 35.13543 80.51939 8/18 15:06 7.62 5.9 76 81.9 109 35.13492 80.51781 8/18 15:37 7.45 6.58 82.5 80.4 ICI TETRA TECH 53 Crooked Creek QUAL2K Model October 15, 2019 ID Latitude(N) Longitude(W) Date Time pH DO(mg/I) DO(%Sat) Temp(°F) 110 35.13382 80.51204 8/18 15:58 7.49 4.65 59 81.5 111 35.13643 80.5126 8/18 16:12 7.69 4.56 58 81.7 112 35.13899 80.51417 8/18 16:24 7.55 4.09 51.7 81.3 113 35.13919 80.51332 8/18 16:34 7.45 5.07 65.2 81.1 114 35.13871 80.51076 8/18 16:42 7.61 5.52 69.8 81.7 115 35.13842 80.50713 8/18 16:50 7.68 5.81 73.4 81.3 116 35.13825 80.50588 8/18 16:56 7.35 5.3 66.5 79.3 Table C-6. Longitudinal data from trip 2 (August 31-September 2, 2016) ID Latitude(N) Longitude(W) Date Time pH DO(mg/I) DO(%Sat) Temp(°F) 120 35.14462 80.47173 8/31 15:02 7.57 6.33 77.4 77.7 121 35.13301 80.4896 8/31 15:26 7.5 7.37 89.1 76.6 122 35.13091 80.49409 8/31 15:49 6.78 7.87 95 76.6 123 35.13112 80.49418 8/31 16:06 7.28 7.29 87.9 76.5 124 35.13121 80.49426 8/31 16:12 7.79 5.03 61.2 77.7 125 35.13803 80.50548 8/31 17:14 7.46 5.17 61.8 76.3 126 35.12832 80.53928 8/31 17:39 6.9 4.26 51.1 76.1 127 no data no data 8/31 18:00 6.62 0.82 9.7 74.3 128 35.10136 80.57244 8/31 18:19 7.07 5.47 66.7 77.7 129 35.10238 80.5838 8/31 18:32 7.18 7.17 88.7 79.2 130 35.09903 80.59232 8/31 18:50 6.98 4.52 54.8 77.2 131 35.0961 80.59836 8/31 19:10 7.27 7.67 95.4 79.2 132 35.09506 80.60077 8/31 19:26 6.78 1.87 22.2 74.8 133 35.10788 80.61561 8/31 19:46 6.8 3 35.9 75.9 134 no data no data 8/31 20:10 7.63 8 98 78.1 135 no data no data 8/31 20:13 7.55 5.9 70.2 75.4 OTETRA TECH 54 Crooked Creek QUAL2K Model October 15, 2019 ID Latitude(N) Longitude(W) Date Time pH DO(mg/I) DO(%Sat) Temp(°F) 136 35.13803 80.50533 9/1 8:13 7.29 4.66 55 74.1 137 35.13571 80.5023 9/1 8:30 7.42 5.59 65.4 73.9 138 35.13332 80.50132 9/1 8:42 7.33 5.79 67.8 73.6 139 35.13187 80.49962 9/1 9:15 7.45 5.9 68.3 73.6 140 35.13139 80.49867 9/1 9:23 7.39 6.51 76.1 73.4 141 35.13094 80.49665 9/1 9:41 7.47 6.45 75.5 73.8 142 35.13089 80.49506 9/1 9:50 7.43 6.81 79.7 73.6 143 35.13116 80.49414 9/1 9:57 7.31 7.35 87.5 75.2 144 35.13094 80.49404 9/1 10:01 6.23 2.67 30.7 71.1 145 35.13134 80.49369 9/1 10:05 7.34 5.87 68.7 73.8 146 35.13165 80.49204 9/1 10:14 7.28 4.65 54.6 73.9 148 35.13233 80.4902 9/1 10:26 7.34 4.96 58.7 74.3 149 35.13306 80.48958 9/1 10:35 7.38 6 70.8 74.7 150 35.1341 80.48951 9/1 10:41 7.47 6.12 72.3 74.7 151 35.13606 80.48993 9/1 10:50 7.35 6.02 70.9 74.3 152 35.13813 80.49062 9/1 11:00 7.45 5.52 65.3 74.7 154 35.13709 80.48772 9/1 11:20 7.63 7.24 86.2 75.4 156 35.13804 80.4855 9/1 11:36 7.6 6.72 79.5 74.7 158 35.14062 80.48538 9/1 12:00 7.54 7.43 87.6 74.5 159 35.14259 80.48672 9/1 12:09 7.44 4.66 54.8 74.1 160 35.14266 80.48602 9/1 12:18 7.42 5.99 71.3 75.2 161 35.14226 80.48444 9/1 12:49 7.23 5.01 60.1 75.9 163 35.14281 80.4832 9/1 13:20 7.26 6.56 79.3 76.8 165 35.1444 80.48367 9/1 13:39 7.47 7.42 91.7 78.6 167 35.14518 80.48033 9/1 13:50 7.24 5.8 69.7 76.3 ®TETRA TECH 55 Crooked Creek QUAL2K Model October 15, 2019 ID Latitude(N) Longitude (W) Date Time pH DO(mg/I) DO(%Sat) Temp (°F) 168 35.14437 80.47944 9/1 14:00 7.4 6.17 75.5 78.1 169 35.14214 80.47688 9/1 14:12 7.3 4.67 56.3 77.4 171 35.14138 80.47367 9/1 14:30 7.57 8.05 99.7 79.2 172 35.14304 80.47221 9/1 14:37 7.71 7.87 97.5 79.2 173 35.14477 80.47175 9/1 14:50 7.71 6.54 81.3 79.5 174 35.14561 80.4708 9/1 16:04 7.85 6.37 80.2 80.8 176 35.14824 80.46992 9/1 16:15 7.54 7.77 98.4 81.3 177 35.14809 80.46889 9/1 16:23 7.62 7.55 95.5 81.3 178 35.1466 80.46709 9/1 4:32 7.6 7.23 89.5 79.2 180 35.14716 80.46584 9/1 16:44 7.66 6.45 80.8 80.4 181 35.14845 80.46641 9/1 16:48 7.6 6.7 83 79.2 182 35.15091 80.46693 9/1 16:57 7.66 6.14 76.5 79.9 183 35.15145 80.46413 9/1 17:23 7.75 6.47 80.7 79.9 185 35.14817 80.46246 9/1 17:35 7.85 7.65 94.8 79.2 187 35.14616 80.46063 9/1 17:46 7.8 6.98 86 78.8 188 35.15005 80.45959 9/1 17:57 7.91 6.67 82 78.4 189 35.14981 80.45807 9/1 18:10 7.89 5.28 64.9 78.4 Table C-7. Longitudinal data from trip 3 (September 13-16, 2016) Specific ID Latitude Longitude Date Time Turbidity pH DO DO Conductivity Temp (N) (W) (NTU) (mg/I) (%Sat) (uS/cm) (°F) 194 35.14474 80.47161 9/14 7:20 6.4 6.53 6.23 71 159 71.1 195 35.13801 80.50545 9/14 7:46 7.4 6.07 6.27 71.6 169.1 71.4 196 35.10223 80.58383 9/14 8:20 10.1 6.48 4.69 54.7 531 73.4 197 35.10636 80.54846 9/14 9:20 11.8 5.95 0.57 6.5 102.2 71.6 198 35.10777 80.548 9/14 9:26 65 6.39 0.09 1.1 103 71.8 [ TETRA TECH 56 Crooked Creek QUAL2K Model October 15, 2019 Specific ID Latitude Longitude Date Time Turbidity pH DO oD0 Conductivity Temp (N) (W) (NTU) (mg/I) (/oSat) (uS/cm) ( F) 199 35.10886 80.54678 9/14 9:40 13.3 6.61 0.28 3.3 105.1 71.2 200 35.11024 80.54744 9/14 10:02 43 6.59 0.05 0.6 136 71.6 201 35.11235 80.54677 9/14 10:19 10.3 6.79 0.29 3.4 102 71.1 203 35.11274 80.54707 9/14 10:36 12.6 7.09 5.62 65.6 498 73.4 204 35.11332 80.54606 9/14 10:50 11.7 7.16 4.99 58.3 499 73.4 205 35.11466 80.54564 9/14 11:03 15.9 7.17 4.3 50.4 489 73.8 206 35.11606 80.54512 9/14 11:20 19.9 7.07 3.44 40.4 459 73.8 207 35.11754 80.54533 9/14 11:29 33.1 7.02 2.51 29.4 420 73.8 208 35.11809 80.54537 9/14 11:38 28.2 7.02 3.25 37.9 398 73.6 209 35.11847 80.54442 9/14 11:47 14.5 7.05 3.27 38.2 406 73.4 210 35.11859 80.5431 9/14 11:58 12.7 7.05 3.07 36 402 73.8 211 35.11815 80.54212 9/14 12:13 25.4 7.03 3.25 38.6 396 74.3 212 35.11897 80.54178 9/14 12:22 17.4 7.15 3.76 44.1 391 73.8 213 35.12085 80.54262 9/14 12:56 11.2 7.09 2.95 34.3 384 73.0 214 35.12205 80.54395 9/14 13:05 12 7.01 2.98 35 379 73.8 215 35.12263 80.54272 9/14 13:10 39.9 6.98 2.07 24.3 353 73.0 216 35.1223 80.542 9/14 13:14 42.6 6.91 1.67 19.5 337 73.0 217 35.12228 80.54147 9/14 13:23 90 7.02 5.07 59.7 334 74.5 218 35.12233 80.54047 9/14 13:29 29 7.16 5.7 67.5 332 74.8 219 35.1226 80.53941 9/14 13:35 20.9 7.21 6.08 72.2 331 75.0 220 35.12211 80.5386 9/14 13:40 48 7.25 6.14 72.3 331 74.3 221 35.12314 80.5385 9/14 13:50 12.4 7.2 5.58 65.6 333 73.9 222 35.1237 80.53819 9/14 13:57 25.5 7.23 5.76 67.9 335 74.3 223 35.12588 80.53824 9/14 14:08 21.5 7.19 5.15 60.1 344 73.4 224 35.12732 80.53961 9/14 14:18 17.8 7.28 4.98 58.6 339 74.3 ®TETRA TECH 57 Crooked Creek QUAL2K Model October 15, 2019 Specific ID Latitude Longitude Date Time Turbidity pH DO DO Conductivity Temp o (N) (W) (NTU) (mg/I) (%Sat) (uS/cm) ( F) 225 35.12815 80.53922 9/14 14:24 21.4 7.31 4.73 55.7 333 74.1 226 35.12886 80.53698 9/14 14:30 26.4 7.28 4.61 54.1 314 74.1 227 35.13293 80.48951 9/14 15:12 4.5 7.71 8.14 99.3 188 77.7 228 35.13092 80.49402 9/14 15:24 0.1 7.51 18.9 229 263 76.8 229 35.13119 80.49428 9/14 15:31 0.8 7.56 7.8 94.3 837 76.6 230 no data no data 9/14 16:02 6.9 7.54 7.05 85.1 575 76.5 231 35.09909 80.59237 9/14 16:17 5.6 7.14 5.58 66.8 5.79 75.9 232 35.09612 80.59837 9/14 16:42 3 7.18 7.75 94.7 628 77.7 233 35.09518 80.60079 9/14 16:51 49 7.28 1.63 18.7 198 72.1 234 35.10787 80.61551 9/14 17:07 43.3 7.22 2.68 31.1 274 72.7 235 35.1042 80.63397 9/14 17:19 0.4 7.06 8.16 98.1 641 76.1 236 35.10434 80.63426 9/14 17:24 54.4 7.29 2.92 33.6 125 72.1 237 35.1288 80.537 9/15 7:30 14.9 7.47 4.44 51.2 330 72.1 238 35.12906 80.53555 9/15 7:38 11.6 7.29 4.31 49.6 332 72.0 239 35.12732 80.53225 9/15 7:48 12.2 7.2 3.54 41 313 72.5 240 35.12809 80.53156 9/15 7:56 8.5 7.19 3.55 40.9 299 72.1 241 35.12933 80.5312 9/15 8:04 4.5 7.33 5.86 67 294 71.4 242 35.1295 80.53051 9/15 8:09 23.4 7.37 5.89 67.2 293 71.2 243 35.12904 80.52917 9/15 8:15 16.9 7.35 5.36 61.2 291 71.4 244 35.1277 80.52801 9/15 8:24 8.5 7.35 5.09 58.6 291 72.1 245 35.12745 80.52695 9/15 8:34 8.5 7.34 5.14 59.3 279 72.5 246 35.1299 80.52703 9/15 8:48 10.1 7.41 6.18 70.6 274 71.4 247 35.13115 80.52707 9/15 8:56 5.1 7.44 6.29 71.7 271 71.1 248 35.13271 80.5256 9/15 9:03 4.8 7.43 5.71 65.6 266 71.8 249 35.13482 80.52454 9/15 9:10 10.2 7.33 4.98 57.7 238 72.9 OTETRA TECH 58 Crooked Creek QUAL2K Model October 15, 2019 ID Latitude Longitude Date Time Turbidity pH DO DO Specific Conductivity Temp (N) (W) (NTU) (mg/I) (%Sat) (uS/cm) (°F) 250 35.13532 80.523 9/15 9:30 22.5 7.38 6.29 72.8 237 72.7 251 35.13454 80.52183 9/15 9:41 18.3 7.47 6.72 77.4 234 72.3 252 35.13451 80.52116 9/15 10:00 10.6 7.46 6.45 74.1 233 72.0 253 35.13541 80.51936 9/15 10:20 5 7.55 6.41 73.2 231 71.4 254 35.13516 80.51765 9/15 10:25 14.1 7.43 5.36 61.6 229 71.8 255 35.13304 80.51588 9/15 10:35 11.9 7.5 5.56 64.6 213 72.9 256 35.13282 80.51525 9/15 10:40 10.4 7.41 5.48 63.5 210 72.9 257 35.1327 80.51311 9/15 10:52 9.7 7.4 5.2 60.4 206 73.0 258 no data no data 9/15 10:58 7.9 7.67 6.01 69.6 205 72.7 259 35.13502 80.51162 9/15 11:17 10.9 7.34 5.77 66.8 199 72.7 260 35.13643 80.51194 9/15 11:23 no data 7.73 6.99 80.7 198 72.5 261 35.13703 80.51332 9/15 11:31 10.2 7.48 6.62 76.2 197 72.1 262 35.13924 80.51406 9/15 11:43 10.3 7.33 4.65 54 185 73.0 263 35.13919 80.5123 9/15 11:53 8.5 7.52 6.23 72.5 185 73.2 264 no data no data 9/15 11:55 7.4 7.45 6.45 75.1 186 73.0 265 no data no data 9/15 11:58 14.9 7.43 6.74 78.8 183 73.6 266 35.13913 80.51331 9/15 12:02 16.8 7.29 6.03 70.7 183 73.9 267 35.13929 80.51405 9/15 12:06 43.1 7.36 5.96 70.1 184 74.1 268 35.13933 80.51427 9/15 12:09 12.5 7.3 4.92 57.4 185 73.4 269 35.13878 80.51134 9/15 12:40 10.9 7.89 6.82 79.8 183 73.8 270 35.13878 80.51134 9/15 12:45 4.8 7.28 3.12 36.3 154 72.7 271 no data no data 9/15 12:52 4 7.57 7.05 82.2 175 73.2 272 35.13826 80.51035 9/15 12:54 5.9 7.6 7.31 86.2 183 74.3 273 35.13817 80.50831 9/15 13:06 17.2 7.63 7.65 89.2 180 73.4 274 35.13847 80.50727 9/15 13:11 6.5 7.66 7.93 92.6 180 73.6 ICI TETRA TECH 59 Crooked Creek QUAL2K Model October 15, 2019 Specific ID Latitude Longitude Date Time Turbidity pH DO oD0 Conductivity Temp (N) (W) (NTU) (mg/I) (/oSat) (uS/cm) ( F) 275 no data no data 9/15 13:22 11.9 7.52 7.1 82.4 178 72.9 276 no data no data 9/15 13:28 7.1 7.39 5.82 68.6 174 74.3 277 35.13634 80.5026 9/15 13:39 10.7 7.82 8.13 97.4 171 76.1 278 35.13442 80.5015 9/15 13:46 13.1 7.84 8.56 102.1 169 75.7 279 35.13269 80.50138 9/15 13:57 7.1 7.88 8.94 108.3 167 77.2 280 35.13197 80.49989 9/15 14:02 6.6 7.89 8.5 101.7 166 75.9 281 35.13145 80.4984 9/15 14:10 9.3 7.7 8.1 95.6 166 74.5 282 35.1309 80.49506 9/15 14:19 8.6 7.87 8.91 107.1 164 76.3 283 35.13115 80.49435 9/15 14:23 11.9 7.58 5.73 65.8 166 72.5 284 35.13125 80.4938 9/15 14:26 16 7.72 8.82 105.4 253 75.7 285 35.13105 80.49401 9/15 14:29 0.1 7.63 16.7 197 269 74.7 286 35.13116 80.4942 9/15 14:32 1.9 7.54 7.84 94.5 790 76.3 C.4 DIURNAL DISSOLVED OXYGEN Daily cycles of dissolved oxygen concentration can vary due to temperature, macrophyte productivity, and changes in point sources. Diurnal DO was measured using long-term sondes for multiple days at a number of locations along Crooked Creek at ten-minute intervals. The sampling locations for each trip are shown in Figure C-5, with overall statistics reported in Table C-8. Timeseries results of all results for all sites (not temperature-corrected) are seen in Figure C-6, Figure C-7, and Figure C-8. Table C-8. Dissolved oxygen sonde result statistics (units are mg/L) Trip Site Average DO Minimum DO Maximum DO DO Range 1 DS of CC#2 4.46 3.60 5.12 1.52 (8/13-8/19) HWY 601 3.15 2.54 3.72 1.18 US of CC#2 2.03 1.01 3.25 2.24 2 Brief Rd 4.97 4.11 6.28 2.17 (8/31-9/2) SR 1601 4.52 3.30 5.83 2.53 „pi, TETRA TECH 60 Crooked Creek QUAL2K Model October 15, 2019 Trip Site Average DO Minimum DO Maximum DO DO Range HWY 601 3.47 2.82 5.01 2.19 3 Brief Rd 3.93 3.30 4.94 1.64 (9/13-9/16) N Rocky River 4.89 3.54 6.70 3.16 Rd SR 1601 4.67 3.33 6.33 3.00 Brief Road SR 1601 HWY 601 t t DS of CC#2 US of CC#2 Rocky River Rd +r,41.114.4)11) ::ty 411kifr J Legend °°� II Sonde Location(8/13-8/19) , t - 0 Sonde Location(8/31-9/2) Sonde Location(9/13-9/16) • WWTP Discharge Crooked Creek Watershed N 0 05 , 2 _. NHD HiRes Flowline ®TETRA TECH Dissolved Oxygen Sonde Sites n —K10R181ef N oos z� n Watershed Boundary WO w�an. eaory Camino cns awo.rw OMiles Figure C-5. Dissolved oxygen monitoring sonde sites (all trips) ®TETRA TECH 61 Crooked Creek QUAL2K Model October 15, 2019 8 7 5 O -0• 4 O 11.191111111411.111.111.1114111111111111.111114111)%040001. • 1 111111111111144101. 0 8/15/16 13:00 8/16/16 1:00 8/16/16 13:00 8/17/16 1:00 8/17/16 13:00 8/18/16 1:00 •Trip 1:US of CC#2 •Trip 1:DS from CC#2 •Trip 1:HWY 601 Figure C-6. Diurnal dissolved oxygen concentrations (8/15-8/19), gray areas are night(7pm-7am) 8 7 6 • 1 • • • • •• • A. • O • • I4 Y P •'•• • • • 4 • • v Co) 0 2 1 0 8/31 16:49 8/3121:37 9/12:25 9/17:13 9/112:01 9/116:49 9/121:37 9/2 2:25 9/2 7:13 •Tri 2:Brief Rd •Tri 2:SR 1601 •Trip 2:HWY 601 Figure C-7. Diurnal dissolved oxygen concentrations (8/31-9/2), gray areas are night(7pm-7am) TETRA TECH 62 Crooked Creek QUAL2K Model October 15, 2019 8 • 6 ~ s = eil 04 • 0 • •• a.) • • O 3 2 1 0 9/14 7:00 9/14 11:48 9/14 16:36 9/14 21:24 9/15 2:12 9/15 7:00 9/15 11:48 9/15 16:36 •Trip 3:Brief Rd •Trip 3:N Rocky River Rd •Trip 3:SR 1601 Figure C-8. Diurnal dissolved oxygen concentrations (9/13-9/16), gray areas are night(7pm-7am) ( TETRA TECH 63 Hazen Attachment B: Crooked Creek Model Application for Grassy Branch Wastewater Treatment Plant, Tetra Tech, October 15, 2019 (Note: Report was revised per comments from Division of Water Resources per meeting on October 1, 2019) Crooked Creek QUAL2K Model Application for Grassy Branch WWTP Union County, North Carolina December 4, 2019 PREPARED FOR PREPARED BY Union County Public Works Tetra Tech 500 North Main Street, Suite 500 One Park Drive, Suite 200 Monroe. NC 28112 PO Box 14409 Research Triangle Park. NC 27709 •.: 4r •� S `A i•' •A. • • Pictured:North Fork Crooked Creek(Tetra Tech. 2016) TETRA TECH (This page was intentionally left blank.) TABLE OF CONTENTS 1.0 INTRODUCTION 1 2.0 QUAL2K MODEL APPLICATION SET-UP 3 2.1 Simulating Critical Conditions 3 2.1.1 Critical Low Flow Statistics 3 2.1.2 Modified Seasonal Inputs 4 2.1.3 Permitted Discharge Assumptions 6 3.0 MODIFIED DISCHARGE CONDITIONS SCENARIO RESULTS 8 3.1 Model Application Sensitivity Testing 9 3.2 Instream Ammonia Toxicity 9 3.3 Instream TSS and Turbidity 10 LIST OF TABLES Table 1. Estimated 7Q10 flow tabulated for boundary conditions of Crooked Creek. 3 Table 2. Existing point source permit limits for water treatment facilities along Crooked Creek. 6 Table 3. Proposed SOC and final effluent permit limits for Grassy Branch VWVTP (NC0085812) 6 Table 4. Effluent water temperature for seasonal simulations. 7 Table 5. Crooked Creek QUAL2K model scenarios results for summer and winter critical conditions. 8 Table 6. Crooked Creek QUAL2K model scenarios sensitivity testing. 9 Table 7. Crooked Creek QUAL2K model application scenario results for ammonia toxicity. 10 Table 8. Crooked Creek QUAL2K model application scenario results for instream TSS concentration 11 LIST OF FIGURES Figure 1. Crooked Creek watershed location map, model segmentation, and VVVVTP discharge sites. 2 Figure 2. Crooked Creek QUAL2K model 7Q10 flow balance schematic diagram 4 Figure 3. Crooked Creek QUAL2K model scenario results for summer and winter. 8 ®TETRA TECH � Crooked Creek Model Application for Grassy Branch WWTP-Union County December 4, 2019 1.0 INTRODUCTION This technical modeling memo is intended to accompany Union County's request for receiving a Special Order by Consent(SOC) from the North Carolina Division of Water Resources for the Grassy Branch Wastewater Treatment Plant(WWTP). The facility (NPDES Permit No. NC0085812) discharges into Crooked Creek approximately seven river miles upstream of the confluence with the Rocky River in the Yadkin-Pee Dee River Basin. The Grassy Branch WWTP has exhibited periodic noncompliance with existing effluent NPDES permit limits. The County is seeking interim limits under the SOC and this memo summarizes our findings of a modeling assessment performed to evaluate potential impacts on the receiving waters of the proposed interim limits. A QUAL2K model for Crooked Creek was used for the modeling assessment. The model was calibrated and corroborated based on data collected in 2016 (Tetra Tech, 20191). The QUAL2K model development report and corresponding Excel files were submitted to the North Carolina Division of Water Resources (DWR) on August 12-13, 2019 and verbal approved was received in-person from DWR staff on October 1, 2019. For this SOC modeling analysis, the calibrated QUAL2K model was setup to simulate seasonally critical conditions and maximum permitted effluent discharges for all treatment facilities located along Crooked Creek. This report details the QUAL2K model application and SOC scenario analysis. 1 Tetra Tech. 2019. Crooked Creek QUAL2K Model Development; Union County, North Carolina. Prepared for Union County Public Works, Monroe, NC. 1 ( I TETRA TECH Crooked Creek QUAL2K Model Application for Grassy Branch VWVTP-Union County December 4, 2019 ,Rocky River Crooked Creek Grassy Branch WWTP Hemby Acres WWTP North Fork Crooked Creek, u Crooked Creek WWTP#2- Grassy Branch S' t r .... Legend .wonr _ WWTP Discharge ® Large Beaver Dam South Fork Crooked Creek Riveustream \-,\_,..„..„,..x,-----f-ri QWatershed Boundary Model Reach Reach t ® Reach 2 -- —,- Reach 3 eaeeee� Reach 4 Crooked Creek Watershed N o 0 5 1 2 - Reach s It TETRA TECH QUAL2K Model Segmentation A OKilometers 0 0 5 1 2 -— Roach e vw_n455 suww.nvaary cIPS 3240_r..r Miles u.owmcedcic.aoi7 Hrtna.. Figure 1. Crooked Creek watershed location map, model segmentation, and WWTP discharge sites. [It) TETRA TECH 2 Crooked Creek QUAL2K Model Application for Grassy Branch WWTP-Union County December 4, 2019 2.0 QUAL2K MODEL APPLICATION SET-UP North Carolina Water Quality Regulations (15A NCAC 02B .0206) specifies that water quality standards related to oxygen-consuming wastes be protected using the minimum average flow for a period of seven consecutive days that has an average recurrence of once in ten years (7Q10 flow). Additionally, the NC regulations (15A NCAC 02B .0404) provide for seasonal variation for the discharge of oxygen-consuming wastes, with the summer period defined as April through October and winter period as November through March. Set-up of the Crooked Creek QUAL2K model for evaluating impacts under seasonal critical conditions is documented below. 2.1 SIMULATING CRITICAL CONDITIONS 2.1.1 Critical Low Flow Statistics There are very limited flow gage records within the Crooked Creek watershed. Curtis Weaver of USGS provided 7Q10 estimates for the watershed based on a drainage area relationship of 0.001 cubic feet per square mile (cfsm) derived from the nearby Richardson Creek and Crooked Creek monitoring data (USGS, September 2019 via email correspondence). A winter 7Q10 estimate was also provided by Mr. Weaver as one order of magnitude greater, at 0.01 cfsm. Mr. Weaver provided 7Q10 flow estimates based on drainage area at Highway 601 and NC Highway 218 of 0.037 cfs and 0.0.044 cfs respectively for summer, and 0.371 cfs and 0.444 cfs respectively for winter. Applying this 7Q10 relationship, flow was calculated at the model boundary inputs for the Crooked Creek QUAL2K model (Table 1). Based on the tributary inflows and the two instream estimates provided by Mr. Weaver, a simple flow balance equation was used to determine the amount of flow which must enter the stream via diffuse baseflow as well (Table 1; Figure 2). Table 1. Estimated 7Q10 flow tabulated for boundary conditions of Crooked Creek. Boundary Condition Drainage Area Summer 7Q10 Winter 7Q10 (mi2) Flow(cfs) Flow (cfs) Headwater 7.4 0.007 0.074 South Fork Crooked Creek (SF CC) tributary 18.4 0.018 0.184 Grassy Branch tributary 3.8 0.004 0.038 Diffuse Flow 1: Headwaters to Highway 601 N/A 0.011 0.113 Diffuse Flow 2: Highway 601 to NC Highway 218 N/A 0.004 0.035 Diffuse Flow 3: NC Highway 218 to Outlet N/A 0.006 0.059 TETRA TECH 3 Crooked Creek QUAL2K Model Application for Grassy Branch WWTP-Union County December 4, 2019 Headwater Inflow Summer 7Q10:0.007 cfs Winter 7Q10:0.074 cfs Diffuse Inflow 1 ► f Summer 7Q10:0.011 cfs SF CC Tributary Winter 7Q10:0.113 cfs Summer 7Q10:0.018 cfs Winter 7Q10:0.184 cfs Highway 601 instream flow Summer 7Q10:0.037 cfs Winter 7Q10:0.371 cfs Grassy Branch Tributary Diffuse Inflow 2 Summer 7Q10:0.004 cfs Summer 7010:0.004 cfs Winter 7Q10:0.038 cfs i Winter 7Q10:0.035 cfs NC Highway 218 instream flow Summer 7Q10:0.044 cfs Winter 7Q10:0.444 cfs Diffuse Inflow 3 Outlet instream flow Summer 7Q10:0.006 cfs Summer 7Q10:0.050 cfs Winter 7Q10:0.059 cfs Winter 7Q10:0.503 cfs v Figure 2. Crooked Creek QUAL2K model 7Q10 flow balance schematic diagram. 2.1.2 Modified Seasonal Inputs 2.1.2.1 Summer Critical Conditions The summer period is identified (per 15A NCAC 02B .0404) in the existing permit as April 1 to October 31. The summer critical conditions model for Crooked Creek is based primarily on the calibration model. Key differences from the calibration model include: • Modification of simulation date based on warmest summer month for water temperature o Meteorological inputs modified based on new simulation date • Modification of boundary conditions (headwaters and tributaries) o Flows to represent critical 7Q10 conditions instream (see Table 1) o Water temperature to represent critically warm summer conditions o DO concentrations to represent median DO saturation observed during critically warm summer conditions • Diffuse inflow conditions were parameterized identically to the headwater boundary conditions All other model inputs were held constant from the calibration model for the summer critical conditions simulation. The warmest summer water temperatures were found to occur in the month of July based on instream water quality data sampling conducted by the Yadkin Pee Dee River Basin Association (YPDRBA) at four sites along Crooked Creek. To parameterize the boundary conditions (headwater, diffuse flow, and tributary inflow), a statistical analysis was conducted on observed instream data measured immediately upstream of the Hemby Acres WWTP. This upstream location is the only water quality sampling site in the basin which is not influenced by an upstream effluent discharge. The 75th percentile water temperature of TETRA TECH 4 Crooked Creek QUAL2K Model Application for Grassy Branch WWTP-Union County December 4, 2019 all measurements at this location (2014-2019) during the month of July was 25.0 °C. The median DO saturation observed during all July measurements of both temperature and DO at this location was 58%. Applying this 58% DO saturation to the water temperature of 25.0 °C results in a boundary condition DO concentration of 4.8 mg/I applied to the headwaters, diffuse, and tributary inflows. QUAL2K requires assignment of a simulation date to support meteorological conditions. The 75th percentile water temperature of 25.0 °C is similar to the average water temperatures observed in July 2015, so the summer critical condition simulation date was selected as July 15, 2015. Meteorological inputs for hourly air and dew point temperatures were pulled from this new simulation date from the same gage as was used for the calibration and corroboration model setup (KNCUNION2 at Campobello Drive). Average air and dew point temperatures on July 15, 2015 are 29.9 °C (85.8 °F) and 19.3 °C (66.7 °F) respectively. 2.1.2.2 Winter Critical Conditions The winter period is identified (per 15A NCAC 02B .0404) in the existing permit as November 1 to March 31. For the winter critical conditions simulation, the following modifications were made relative to the baseline calibration model: • Modification of simulation date based on warmest winter month for water temperature o Meteorological inputs modified based on new simulation date • Modification of boundary conditions (headwaters and tributaries) o Flows to represent winter 7Q10 conditions instream (see Table 1) o Water temperature to represent critically warm winter conditions o DO concentrations to represent median DO saturation observed during critically warm winter conditions • Average shade conditions were decreased by half from 70% to 35% relative to summer conditions to simulate the impact of assumed winter leaf-fall • Diffuse inflow conditions were parameterized identically to the headwater boundary conditions All other model inputs were held constant from the calibration model for the summer critical conditions simulation. Critical winter conditions for water temperature were estimated for boundary conditions using the period of record of instream YPDRBA water quality data. On average, the warmest winter water temperatures occur in the month of November. Water temperature inputs for boundary conditions (headwaters, tributaries, and diffuse inflow) were developed based on the 75th percentile of all observed water temperature results in the POR for the instream water quality sampling site located immediately upstream of Hemby Acres WWTP. The result of this analysis is 13.4 °C, which was applied to all winter critical condition boundary inputs. The median DO saturation observed during all November measurements of both temperature and DO was 67%. Applying this 67% DO saturation to the water temperature of 13.4°C results in a boundary condition DO concentration of 7.0 mg/I. Based on the critical warm water temperature analysis the month of November, the simulation date was selected to be the first of November. The simulate date was selected to be November 1, 2015 as the summer critical condition was also chosen for the year 2015. Meteorological inputs for hourly air and dew point temperatures were pulled from station KNCUNION2. Average air and dew point temperatures on November 1, 2015 are 15.5 °C (59.9 °F) and 13.8 °C (56.9 °F) respectively. [ TETRA TECH 5 Crooked Creek QUAL2K Model Application for Grassy Branch WWTP-Union County December 4, 2019 2.1.3 Permitted Discharge Assumptions There are three permitted point sources located along Crooked Creek modeled explicitly: Hemby Acres WWTP which is operated by Carolina Water Services Inc., Crooked Creek#2 WWTP and Grassy Branch WWTP which are both operated by Union County. For model application scenarios, inputs were based on permitted effluent limitations. Calibration model inputs were held constant for non-permitted constituents (i.e. inorganic and organic phosphorus) for these simulations. Existing permit limits for the three outfalls along Crooked Creek vary seasonally and by facility (Table 2). Due to noncompliance with existing permitted limits for the Grassy Branch WWTP Union County is proposing modified limits for the facility which would reflect an interim SOC period and future final permit limits, both for higher effluent flow conditions (Table 3). Because of the expansion of flow from the facility from 0.05 MGD to 0.12 MGD, permit limits associated with ammonia change from existing permit limits of 2 and 4 mg/I for summer and winter to 1 and 3 mg/I respectively, while the year-round permit limit for DO concentration must stay above 6 mg/I rather than the existing permit limit of 5 mg/I. Discharge Monitoring Report (DMR) data for Grassy Branch WWTP from 2015-2019 includes 184 DO measurements, only 3 of which are below 6 mg/I (2% of samples), so meeting the final permit limit of 6 mg/I for DO should not be an issue for the facility. On average, the WWTP performs with 96% BOD5 removal, 97% TSS removal, and 96% NH3 removal based on DMR records. Similar to the calibration and corroboration model setup, total suspended solids (TSS) is simulated conservatively as inorganic suspended solids (ISS) since organic solids are captured already through the simulation of BOD5 as CBODfast in the model. Table 2. Existing point source permit limits for water treatment facilities along Crooked Creek. NPDES ID Facility Season Flow BOD5 NH3 DO TSS (mg/I) (MGD) (mg/I) (mg/I) (mg/I) Hemby Summer 9 3 NC0035041 Acres 0.3 5 30 Winter 15 8 Crooked Summer 5 2 NC0069841 Creek#2 1.9 >_6 30 Winter 10 4 Grassy Summer 5 2 NC0085812 Branch 0.05 5 30 Winter 10 4 Table 3. Proposed SOC and final effluent permit limits for Grassy Branch WWTP (NC0085812). NH3 DO Permit Note Season Flow (MGD) BOD5 (mgll) (mgll) TSS (mg/I) Summer 6 Interim SOC Limits 0.12 30 ? 5 100 Winter 20 Summer 5 1 Final Limits 0.12 >-6 30 Winter 10 2 CTETRA TECH 6 Crooked Creek QUAL2K Model Application for Grassy Branch VWVTP-Union County December 4, 2019 For summer and winter simulation periods, the following scenarios were simulated: 1. Critical summer conditions, Grassy Branch at interim SOC limits, other outfalls at permit limits 2. Critical summer conditions, Grassy Branch at final permit limits, other outfalls at permit limits 3. Critical winter conditions, Grassy Branch at interim SOC limits, other outfalls at permit limits 4. Critical winter conditions, Grassy Branch at final permit limits, other outfalls at permit limits For the seasonal simulations, the water temperature associated with each effluent discharge point source was developed using the average observed July or November water temperature for 2015 (Table 4). Table 4. Effluent water temperature for seasonal simulations. Facility Summer Water Temperature (°C), Winter Water Temperature (°C), Average July 2015 Average November 2015 Hemby Acres 25.9 14.4 Crooked Creek#2 26.3 18.2 Grassy Branch 25.7 15.9 Note that there is one other permitted discharge for groundwater remediation located near the headwaters of the South Fork Crooked Creek. This permittee (NPDES ID NC0088838) for the Radiator Specialty Company has a maximum permitted discharge limit of 0.09 MGD and monthly water quality limits for the effluent are associated with TSS (30 mg/I), with additional daily maximum limits for a number of pollutants such as tetrachloroethene, vinyl chloride, and dioxane. Although this permitted discharge for groundwater remediation is located far upstream along the South Fork Crooked Creek, the point source was included explicitly in the model at the outlet of South Fork Crooked Creek into the mainstem as permit limits for flow and TSS. Model parameterization for temperature and DO were set equal to those of the South Fork Crooked Creek tributary. [ TETRA TECH 7 Crooked Creek QUAL2K Model Application for Grassy Branch WWTP-Union County December 4, 2019 3.0 MODIFIED DISCHARGE CONDITIONS SCENARIO RESULTS Results for both summer and winter seasonal scenarios indicate that there is assimilative capacity for both interim SOC and final permit limits (Table 5, Figure 3). Although DO concentration is predicted to drop well below the standard in the upper portion of Crooked Creek under critical summer and winter conditions due to extreme low flow and physical channel configuration, the Grassy Branch outfall is well downstream of these locations. The minimum DO concentration downstream of the Grassy Branch WWTP outfall simulated for both interim SOC and final permit limits is predicted to remain above the instream WQS of 5.0 mg/I DO. Table 5. Crooked Creek QUAL2K model scenarios results for summer and winter critical conditions. DO minimum DO at Crooked Scenario Scenario Description downstream of Grassy Creek outlet Branch WWTP (mg/I) (mg/I) Critical summer conditions, Grassy 1 Branch at interim SOC limits, other 5.39 5.89 outfalls at permit limits Critical summer conditions, Grassy 2 Branch at final permit limits, other outfalls 5.53 5.99 at permit limits Critical winter conditions, Grassy Branch 3 at interim SOC limits, other outfalls at 5.66 6.99 permit limits Critical winter conditions, Grassy Branch 4 at final permit limits, other outfalls at 5.76 7.16 permit limits 10.00 Grassy Hemby CC#2 SFCC Beaver Trib 9.00 WWTP WWTP Trib Dams Grassy 1 1 1 1 w�P 8.00 7.00 6.00 --- 5.00 0 4.00 3.00 2.00 1.00 0.00 30.00 25.00 20.00 15.00 10.00 5.00 0.00 Distance from outlet(km) ----WQS -Summer-Interim SOC Limits -Summer-Final Permit Limits Winter-Interim SOC Limits -Winter-Final Permit Limits Figure 3. Crooked Creek QUAL2K model scenario results for summer and winter. TETRA TECH 8 Crooked Creek QUAL2K Model Application for Grassy Branch WWTP-Union County December 4, 2019 3.1 MODEL APPLICATION SENSITIVITY TESTING One area of uncertainty associated with the model application scenarios is related to the level of bottom algae anticipated for critical summer and winter conditions. As mentioned, the model application scenarios were run with bottom algae conditions that were simulated for the calibration model period (bottom algae coverage of 25% for reach 1, and 50% for all other reaches). To test model sensitivity to this parameter, the model application scenarios were run under conditions that bottom algae coverages by reach were increased or decreased by 10% (e.g. reach 1 modified to 15% or 35% coverage, and all other reaches modified to 40% or 60% coverage). Note that on average, this represents a 20 percent change in parameter values (i.e., 10/50 is 0.2 or 20 percent). The results of these sensitivity analyses reveal that even under relative model uncertainty on this parameter, the water quality standard of 5.0 mg/I DO is still met downstream of the Grassy Branch WWTP discharge for all seasonal and effluent conditions (Table 6). Table 6. Crooked Creek QUAL2K model scenarios sensitivity testing. Baseline DO minimum Bottom DO minimum DS Scenario Scenario Description DS of Grassy Branch Algae of Grassy Branch WWTP (mg/I) Coverage WWTP (mg/I) Critical summer conditions, 60% 5.55 Grassy Branch at interim 1 SOC limits, other outfalls at 5.39 permit limits 40% 5.22 Critical summer conditions, 60% 5.71 2 Grassy Branch at future 5.53 permit limits, other outfalls at permit limits 40% 5.34 Critical winter conditions, 60% 5.92 Grassy Branch at interim 3 SOC limits, other outfalls at 5.66 permit limits 40% 5.38 Critical winter conditions, 60% 6.03 Grassy Branch at future 4 permit limits, other outfalls at 5.76 ° permit limits 40/° 5.48 3.2 INSTREAM AMMONIA TOXICITY When effluent flows dominate instream conditions, there can be a concern about ammonia toxicity. For low-flow streams, DWR has set forth a policy that ammonia toxicity is defined as instream concentrations from ammonia exceeding 1.0 mg/I in summer, and 1.8 mg/I in winter. As shown below, for all model application scenarios, ammonia toxicity is not exceeded (Table 7). ®TETRA TECH 9 Crooked Creek QUAL2K Model Application for Grassy Branch WWTP-Union County December 4, 2019 Table 7. Crooked Creek QUAL2K model application scenario results for ammonia toxicity. Maximum NH3 NH3 at Crooked Scenario Scenario Description downstream of Grassy Creek outlet Branch WWTP (mg/I) (mg/I) Critical summer conditions, Grassy 1 Branch at interim SOC limits, other 0.34 0.06 outfalls at permit limits Critical summer conditions, Grassy 2 Branch at final permit limits, other outfalls 0.11 0.06 at permit limits Critical winter conditions, Grassy Branch 3 at interim SOC limits, other outfalls at 1.00 0.04 permit limits Critical winter conditions, Grassy Branch 4 at final permit limits, other outfalls at 0.21 0.03 permit limits 3.3 INSTREAM TSS AND TURBIDITY Turbidity is a measure of water clarity or cloudiness, and the water quality standard in North Carolina for Class C waters is a maximum of 50 Nephelometric Turbidity Units (NTU)2. Although Crooked Creek and its tributaries are not impaired for turbidity, Crooked Creek discharges into the Rocky River which is impaired for turbidity. Key sources of turbidity in the Rocky River watershed have been identified as largely related to stormwater runoff and erosive land use practices which cause sediment wash-off during precipitation events3. Generally, high instream turbidity measurements are associated with precipitation events rather than low- flow conditions which are simulated in this critical conditions QUAL2K model scenario. Model output for TSS can provide some insight into the assimilation of particulate matter instream under low-flow conditions, however the true impact of turbidity instream cannot be captured by this steady-state critical conditions model simulation (Table 8). There are not explicit TSS water quality standards for North Carolina Class C waterways. 2 NC DWR. 2019. NC 15A NCAC 02B Water Quality Standards for Surface Waters. 3 NC DWQ. 2008. Yadkin-Pee Dee River Basin Plan: Rocky River HUC 03040105. ®TETRA TECH 10 Crooked Creek QUAL2K Model Application for Grassy Branch WWTP-Union County December 4, 2019 Table 8. Crooked Creek QUAL2K model application scenario results for instream TSS concentration. Maximum TSS TSS at Crooked Scenario Scenario Description downstream of Grassy Creek outlet Branch WWTP (mg/I) (mg/I) Critical summer conditions, Grassy 1 Branch at interim SOC limits, other 14.50 9.26 outfalls at permit limits Critical summer conditions, Grassy 2 Branch at final permit limits, other outfalls 11.10 8.20 at permit limits Critical winter conditions, Grassy Branch 3 at interim SOC limits, other outfalls at 11.65 6.08 permit limits Critical winter conditions, Grassy Branch 4 at final permit limits, other outfalls at 8.56 5.02 permit limits Turbidity has been measured along Crooked Creek at the four instream YPDRBA sampling sites since 1998. Of the total 913 turbidity measurements, 124 measurements exceed the water quality standard of >_50 NTU, which is 14% of all samples from July 1998 through July 2019. For the period of record at each sampling location, the median turbidity measurement ranges from 14 - 16 NTU, the average ranges from 26-30 NTU, and the maximum measurements range from 298-360 NTU. Paired sampling data of TSS and turbidity are available at YPDRBA site Q8388000 downstream of the Grassy Branch WWTP and tributary on Crooked Creek. The 71 paired samples at this site suggest a generally linear relationship between TSS and turbidity concentrations when analyzed directly, however the relationship is skewed by only 7 paired results for which turbidity results are >_ 50 NTU. When the paired data is transformed using a natural logarithm, the R-squared value for the entire dataset is 0.4, and when turbidity data less than 50 NTU is considered, the R-squared value drops to 0.1. When turbidity measurements are ?. 50 NTU at site Q8388000, TSS measurements range from 15-224 mg/I, which suggests that turbidity violations are not observed when TSS measurements are below 15 mg/I. Although the relationship between turbidity and TSS is weak at this location, simulation results and existing instream data suggest that there is reason to believe that the Grassy Branch WWTP interim SOC and final permit limits will not contribute to turbidity water quality problems during low flow periods. The impact of these permit limits on high flow events are similarly unlikely to contribute to stream turbidity degradation due to the relatively low effluent flow associated with the Grassy Branch WWTP facility relative to instream flows. I I TETRA TECH 11 STATE OF NORTH CAROLINA DEPARTMENT OF ENVIRONMENTAL QUALITY DIVISION OF WATER RESOURES APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT VI. Predicted Compliance Schedule Union County intends to accomplish the following tasks and milestones for the recommended upgrades to the Grassy Branch Wastewater Treatment Plant(WWTP), as follows: Months from Estimated Date from Milestone Notice to Proceed Notice to Proceed ' Submit Contract Documents for 18 months July 2021 regulatory approval for Grassy Branch WWTP Upgrade Project Start construction of Grassy Branch 33 months October 2022 WWTP Upgrade Project upon receiving approval by applicable regulatory agencies Complete construction, start-up and 66 months June 2025 testing of Grassy Branch WWTP Upgrade Project l&I Rehabilitation in Grassy Branch basin ---- On-going ' Note:Estimated completion dates are dependent on date of Notice to Proceed. The Grassy Branch WWTP existing infrastructure will remain in service during the construction of the proposed upgrades. It is not anticipated that construction activity will affect facility performance. STATE OF NORTH CAROLINA DEPARTMENT OF ENVIRONMENTAL QUALITY DIVISION OF WATER RESOURES APPLICATION FOR A SPECIAL ORDER BY CONSENT (SOC) ATTACHMENT VII. Funding Sources Identification Union County intends to fund the recommended improvements and upgrades to the Grassy Branch Wastewater Treatment Plant (WWTP) as follows: Improvement Funding Source Upgrades to Grassy Branch WWTP to increase Funding is available in the Union maximum month design capacity from 0.05 to 0.12 mgd County Public Works Capital Improvements Program I&I Reduction Effort in Grassy Branch basin (on-going) Water and Wastewater Operation and Maintenance funding annually appropriated by the Board of County Commissioners UNION COUNTY DEPARTMENT OF PUBLIC WORKS p 500 North Main Street,Suite 500,Monroe,NC 28112 Phone: (704)296-4210 • Fax:(704)296-4232 May 16, 2019 Mr. W. Corey Basinger Regional Supervisor Water Quality Regional Operations Section Mooresville Regional Office 610 East Center Ave., Suite 301 Mooresville, NC 28115 Dear Mr. Basinger: The purpose of this letter is to confirm Union County's interest in pursuing a Special Order of Consent (SOC) with NCDEQ for flow issues at our Grassy Branch Water Reclamation Facility (WRF). After meeting with our staff on May 2nd, we have been working on developing the information needed to make a formal submission for the SOC. Key to this submission is obtaining technical information from our Engineer who is familiar with the Grassy Branch WRF which will be provided later this month. Once all the needed information is available, we intend to send you a formal SOC application. We appreciate both your and your staff's time and effort in helping us move to a solution for the flow issues at Grassy Branch WRF. Please call me at 704-292-2597 if you need any additional information. Sincerely, Brian Matthews, AICP Assistant County Manager cc: Aubrey Lofton, Interim Public Works Administrator Andrew Neff,Water and Wastewater Division Director Josh Brooks,Asst.Water and Wastewater Division Director Bart Farmer,WRF Superintendent 500 North Main St.,Suite 600 • Monroe, NC 28112-4730 • Phone:(704)296-4210 • Fax: (704)296-4232