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HomeMy WebLinkAbout20240538 Ver 1_More Info Received_20240717 (2)FYZ Civil Calculations Sweetwater Tap Relocation — Culvert Design Duke Energy Hickory, North Carolina July 12, 2024 Duke Energy I Sweetwater Tap Relocation — Culvert Design Calculations ��� Contents Contents Contents ..... 1.0 Project Description.......................................................................................................... 1 2.0 Stormwater Calculations.................................................................................................. 1 2.1 Stormwater Peak Flow and Basin Calculations............................................................ 1 2.2 Stormwater Conveyance.............................................................................................. 1 3.0 Erosion & Sediment Control Calculations........................................................................ 2 Appendices Appendix A — NRCS Soil Survey Appendix B — NOAA Rainfall Data Appendix C — Drainage Area Maps Appendix D — Stormwater Peak Flow Calculations Appendix E — Culvert Calculations Appendix F — Riprap Calculations Duke Energy I Sweetwater Tap Relocation — Culvert Design Calculations ��� Project Description 1.0 Project Description Duke Energy has plans for a gravel access road to facilitate the construction of their Sweetwater Tap Relocation Project in Hickory, North Carolina. In order to construct the gravel access road, a culvert must be installed where the road crosses a tributary to Clark Creek. The tributary is an intermittent stream and the crossing is not located within the FEMA floodplain. 2.0 Stormwater Calculations The stormwater calculations were performed to evaluate the drainage area to the point of interest where the proposed road crosses the tributary to Clark Creek. The drainage area was based on topography form both Lidar survey data and GIS topography. 2.1 Stormwater Peak Flow and Basin Calculations One Point of Interest (POI) was determined for discharge from the site. This POI is located where the proposed road crosses the tributary to Clark Creek. A hydrologic analysis was completed using the NRCS hydrologic method (details for this methodology can be found in the NRCS National Engineering Handbook, Section 4). Drainage area can be seen on the drainage area map in Appendix C Composite curve numbers were calculated for the drainage area utilizing the land cover and the hydrologic soil groups for the site found in the NRCS Soil Survey. The site consists of soils in hydrologic soil groups "A" and "B". The Soil Resource Report for the site can be found in Appendix A. The time of concentration for the existing site drainage area was calculated using TR-55. For the proposed site drainage area, the time of concentration is equal to the time of concentration through the storm conveyance system. The procedure for determining the CN and time of concentration can be found in the NRCS, TR-55, Second Edition, June 1986. A hydrologic routing model was completed using the Bentley HydroCAD software program. The calculated drainage area size, composite curve number and time of concentration for each drainage area were entered into the software. The total rainfall depths for the 10-year, 24-hour design storm event was obtained from the National Oceanic and Atmospheric Administration's website. NOAA rainfall data can be found in Appendix B. The total rainfall depth was entered into the model and run utilizing the NRCS Type 11 rainfall distribution with a one minute time interval. Peak flow for the 10-year design storm was determined to be 93.46 cubic feet per second. The full stormwater peak flow calculations can be found in Appendix D of this report. 2.2 Stormwater Conveyance The culvert capacity calculation was completed using the HY-8 software. HY-8 utilizes the Manning's equation to determine the pipe capacity based on gravity flow and is capable of modeling a culvert embedded in a stream. The pipe design criteria (i.e. pipe length, slope, Duke Energy I Sweetwater Tap Relocation — Culvert Design Calculations ��� Riprap Calculations material/manning's n/embedment) was input into the software based on the design plans. Then a pipe size was selected that would meet the capacity requirement for a 10-yr, 24-hour storm. HY-8 calculations can be seen in Appendix E. 3.0 Riprap Calculations While the goal of the design is to maintain the existing stream hydraulics to the greatest extent possible, the concentration of the site drainage into a culvert for the road crossing will result in a flow exiting the culvert that requires energy dissipation in order to maintain streambed stability. For this design, separate calculations were used to calculate the riprap size and the dimensions of the required riprap. These calculations can be found in Appendix F of this report. Riprap outlet protection for the storm system and BMP outlet culvert were also sized using the results from the storm water conveyance calculations for the 10-year, 24-hour storm event. The appropriate riprap stone size was determined by the using Figure 8.06a from the NCDEQ Erosion and Sediment Control Planning and Design Manual. This figure utilizes the peak discharge to determine the midpoint stone size (D50). For sizing the dimensions of the riprap apron, a spreadsheet was used that accounts for riprap design in a trapezoidal waterway. The outlet protection calculation can be found in Appendix F. Eastern Band of Cherokee Indians I Cherokee Trout Hatc Civil Calculations ��� Appendices Appendix A — NRCS Soil Survey USDA United States Department of Agriculture N RCS Natural Resources Conservation Service A product of the National Cooperative Soil Survey, a joint effort of the United States Department of Agriculture and other Federal agencies, State agencies including the Agricultural Experiment Stations, and local participants Custom Soil Resource Report for Catawba County, North Carolina November 21, 2023 Preface Soil surveys contain information that affects land use planning in survey areas. They highlight soil limitations that affect various land uses and provide information about the properties of the soils in the survey areas. Soil surveys are designed for many different users, including farmers, ranchers, foresters, agronomists, urban planners, community officials, engineers, developers, builders, and home buyers. Also, conservationists, teachers, students, and specialists in recreation, waste disposal, and pollution control can use the surveys to help them understand, protect, or enhance the environment. Various land use regulations of Federal, State, and local governments may impose special restrictions on land use or land treatment. Soil surveys identify soil properties that are used in making various land use or land treatment decisions. The information is intended to help the land users identify and reduce the effects of soil limitations on various land uses. The landowner or user is responsible for identifying and complying with existing laws and regulations. Although soil survey information can be used for general farm, local, and wider area planning, onsite investigation is needed to supplement this information in some cases. Examples include soil quality assessments (http://www.nres.usda.gov/wps/ portal/nres/main/soils/health/) and certain conservation and engineering applications. For more detailed information, contact your local USDA Service Center (https://offices.sc.egov.usda.gov/locator/app?agency=nres) or your NRCS State Soil Scientist (http://www.nres.usda.gov/wps/portal/nres/detail/soils/contactus/? cid=nres142p2_053951). Great differences in soil properties can occur within short distances. Some soils are seasonally wet or subject to flooding. Some are too unstable to be used as a foundation for buildings or roads. Clayey or wet soils are poorly suited to use as septic tank absorption fields. A high water table makes a soil poorly suited to basements or underground installations. The National Cooperative Soil Survey is a joint effort of the United States Department of Agriculture and other Federal agencies, State agencies including the Agricultural Experiment Stations, and local agencies. The Natural Resources Conservation Service (NRCS) has leadership for the Federal part of the National Cooperative Soil Survey. Information about soils is updated periodically. Updated information is available through the NRCS Web Soil Survey, the site for official soil survey information. The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, age, disability, and where applicable, sex, marital status, familial status, parental status, religion, sexual orientation, genetic information, political beliefs, reprisal, or because all or a part of an individual's income is derived from any public assistance program. (Not all prohibited bases apply to all programs.) Persons with disabilities who require 2 alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA's TARGET Center at (202) 720-2600 (voice and TDD). To file a complaint of discrimination, write to USDA, Director, Office of Civil Rights, 1400 Independence Avenue, S.W., Washington, D.C. 20250-9410 or call (800) 795-3272 (voice) or (202) 720-6382 (TDD). USDA is an equal opportunity provider and employer. 3 Contents Preface.................................................................................................................... 2 How Soil Surveys Are Made..................................................................................5 SoilMap.................................................................................................................. 8 SoilMap................................................................................................................9 Legend................................................................................................................10 MapUnit Legend................................................................................................ 11 MapUnit Descriptions.........................................................................................11 Catawba County, North Carolina.................................................................... 14 CfB—Clifford sandy loam, 2 to 6 percent slopes.........................................14 CfC—Clifford sandy loam, 6 to 10 percent slopes ...................................... 15 CgB2—Clifford sandy clay loam, 2 to 6 percent slopes, moderately eroded...................................................................................................16 CgC2—Clifford sandy clay loam, 6 to 10 percent slopes, moderately eroded...................................................................................................18 CsA—Codorus loam, 0 to 2 percent slopes, frequently flooded..................19 FaE3—Fairview clay loam, 10 to 25 percent slopes, severely eroded ........ 21 FcC—Fairview gravelly fine sandy loam, 6 to 10 percent slopes................22 FdE2—Fairview soils, 10 to 25 percent slopes, moderately eroded........... 23 TmC—Tomlin loam, 6 to 10 percent slopes ................................................ 24 References............................................................................................................ 26 4 How Soil Surveys Are Made Soil surveys are made to provide information about the soils and miscellaneous areas in a specific area. They include a description of the soils and miscellaneous areas and their location on the landscape and tables that show soil properties and limitations affecting various uses. Soil scientists observed the steepness, length, and shape of the slopes; the general pattern of drainage; the kinds of crops and native plants; and the kinds of bedrock. They observed and described many soil profiles. A soil profile is the sequence of natural layers, or horizons, in a soil. The profile extends from the surface down into the unconsolidated material in which the soil formed or from the surface down to bedrock. The unconsolidated material is devoid of roots and other living organisms and has not been changed by other biological activity. Currently, soils are mapped according to the boundaries of major land resource areas (MLRAs). MLRAs are geographically associated land resource units that share common characteristics related to physiography, geology, climate, water resources, soils, biological resources, and land uses (USDA, 2006). Soil survey areas typically consist of parts of one or more MLRA. The soils and miscellaneous areas in a survey area occur in an orderly pattern that is related to the geology, landforms, relief, climate, and natural vegetation of the area. Each kind of soil and miscellaneous area is associated with a particular kind of landform or with a segment of the landform. By observing the soils and miscellaneous areas in the survey area and relating their position to specific segments of the landform, a soil scientist develops a concept, or model, of how they were formed. Thus, during mapping, this model enables the soil scientist to predict with a considerable degree of accuracy the kind of soil or miscellaneous area at a specific location on the landscape. Commonly, individual soils on the landscape merge into one another as their characteristics gradually change. To construct an accurate soil map, however, soil scientists must determine the boundaries between the soils. They can observe only a limited number of soil profiles. Nevertheless, these observations, supplemented by an understanding of the soil -vegetation -landscape relationship, are sufficient to verify predictions of the kinds of soil in an area and to determine the boundaries. Soil scientists recorded the characteristics of the soil profiles that they studied. They noted soil color, texture, size and shape of soil aggregates, kind and amount of rock fragments, distribution of plant roots, reaction, and other features that enable them to identify soils. After describing the soils in the survey area and determining their properties, the soil scientists assigned the soils to taxonomic classes (units). Taxonomic classes are concepts. Each taxonomic class has a set of soil characteristics with precisely defined limits. The classes are used as a basis for comparison to classify soils systematically. Soil taxonomy, the system of taxonomic classification used in the United States, is based mainly on the kind and character of soil properties and the arrangement of horizons within the profile. After the soil 5 Custom Soil Resource Report scientists classified and named the soils in the survey area, they compared the individual soils with similar soils in the same taxonomic class in other areas so that they could confirm data and assemble additional data based on experience and research. The objective of soil mapping is not to delineate pure map unit components; the objective is to separate the landscape into landforms or landform segments that have similar use and management requirements. Each map unit is defined by a unique combination of soil components and/or miscellaneous areas in predictable proportions. Some components may be highly contrasting to the other components of the map unit. The presence of minor components in a map unit in no way diminishes the usefulness or accuracy of the data. The delineation of such landforms and landform segments on the map provides sufficient information for the development of resource plans. If intensive use of small areas is planned, onsite investigation is needed to define and locate the soils and miscellaneous areas. Soil scientists make many field observations in the process of producing a soil map. The frequency of observation is dependent upon several factors, including scale of mapping, intensity of mapping, design of map units, complexity of the landscape, and experience of the soil scientist. Observations are made to test and refine the soil -landscape model and predictions and to verify the classification of the soils at specific locations. Once the soil -landscape model is refined, a significantly smaller number of measurements of individual soil properties are made and recorded. These measurements may include field measurements, such as those for color, depth to bedrock, and texture, and laboratory measurements, such as those for content of sand, silt, clay, salt, and other components. Properties of each soil typically vary from one point to another across the landscape. Observations for map unit components are aggregated to develop ranges of characteristics for the components. The aggregated values are presented. Direct measurements do not exist for every property presented for every map unit component. Values for some properties are estimated from combinations of other properties. While a soil survey is in progress, samples of some of the soils in the area generally are collected for laboratory analyses and for engineering tests. Soil scientists interpret the data from these analyses and tests as well as the field -observed characteristics and the soil properties to determine the expected behavior of the soils under different uses. Interpretations for all of the soils are field tested through observation of the soils in different uses and under different levels of management. Some interpretations are modified to fit local conditions, and some new interpretations are developed to meet local needs. Data are assembled from other sources, such as research information, production records, and field experience of specialists. For example, data on crop yields under defined levels of management are assembled from farm records and from field or plot experiments on the same kinds of soil. Predictions about soil behavior are based not only on soil properties but also on such variables as climate and biological activity. Soil conditions are predictable over long periods of time, but they are not predictable from year to year. For example, soil scientists can predict with a fairly high degree of accuracy that a given soil will have a high water table within certain depths in most years, but they cannot predict that a high water table will always be at a specific level in the soil on a specific date. After soil scientists located and identified the significant natural bodies of soil in the survey area, they drew the boundaries of these bodies on aerial photographs and 0 Custom Soil Resource Report identified each as a specific map unit. Aerial photographs show trees, buildings, fields, roads, and rivers, all of which help in locating boundaries accurately. 7 Soil Map The soil map section includes the soil map for the defined area of interest, a list of soil map units on the map and extent of each map unit, and cartographic symbols displayed on the map. Also presented are various metadata about data used to produce the map, and a description of each soil map unit. 0 Custom Soil Resource Report Soil Map o 471000 471100 471200 471300 4714W 471500 471600 471700 4718M 4719M 472000 472100 472200 472300 472400 472500 35' 43' 32" N f _. 35' 43' 32" N 8 �^ 4. •. 8 If ell 3 KILN / f j _ 35° 42' S9" N 35° 47 59" N 471000 471100 471200 471300 471400 471500 471600 471700 471800 471900 472000 472100 472200 472300 472400 472500 3 3 a - Map Scale: 1:7,180 i printed on A landscape (11" x 8.5") sheet. Meteso o N 0 100 200 400 600 reef 0 300 600 1200 1800 Map projection: Web Mercator Comer coordinates: WGS84 Edge tics: UTM Zone 17N WGS84 9 MAP LEGEND Area of Interest (AOI) Area of Interest (AOI) Soils 0 Soil Map Unit Polygons im 0 Soil Map Unit Lines ■ Soil Map Unit Points Special Point Features Blowout Borrow Pit Clay Spot Closed Depression Gravel Pit .4 Gravelly Spot 0 Landfill Lava Flow Marsh or swamp + Mine or Quarry Miscellaneous Water Perennial Water Rock Outcrop Saline Spot d Sandy Spot Severely Eroded Spot Sinkhole Slide or Slip Sodic Spot Custom Soil Resource Report MAP INFORMATION A Spoil Area The soil surveys that comprise your AOI were mapped at 1:15,800. Stony Spot Very Stony Spot Warning: Soil Map may not be valid at this scale. Wet Spot Enlargement of maps beyond the scale of mapping can cause Other misunderstanding of the detail of mapping and accuracy of soil .- Special Line Features line placement. The maps do not show the small areas of contrasting soils that could have been shown at a more detailed Water Features scale. - Streams and Canals Transportation Please rely on the bar scale on each map sheet for map �}} Rails measurements. Interstate Highways Source of Map: Natural Resources Conservation Service US Routes Web Soil Survey URL: Coordinate System: Web Mercator (EPSG:3857) Major Roads Local Roads Maps from the Web Soil Survey are based on the Web Mercator projection, which preserves direction and shape but distorts Background distance and area. A projection that preserves area, such as the Aerial Photography Albers equal-area conic projection, should be used if more accurate calculations of distance or area are required. This product is generated from the USDA-NRCS certified data as of the version date(s) listed below. Soil Survey Area: Catawba County, North Carolina Survey Area Data: Version 24, Sep 13, 2023 Soil map units are labeled (as space allows) for map scales 1:50,000 or larger. Date(s) aerial images were photographed: Apr 22, 2022—May 10, 2022 The orthophoto or other base map on which the soil lines were compiled and digitized probably differs from the background imagery displayed on these maps. As a result, some minor shifting of map unit boundaries may be evident. 10 Custom Soil Resource Report Map Unit Legend Map Unit Symbol Map Unit Name Acres in AOI Percent of AOI CfB Clifford sandy loam, 2 to 6 49.6 27.5% percent slopes Clifford sandy loam, 6 to 10 CfC 10.9 6.1% percent slopes CgB2 Clifford sandy clay loam, 2 to 6 0.7 0.4% percent slopes, moderately eroded CgC2 Clifford sandy clay loam, 6 to 10 5.6 3.1 % percent slopes, moderately eroded CsA Codorus loam, 0 to 2 percent 12.8 7.1 % slopes, frequently flooded FaE3 Fairview clay loam, 10 to 25 5.0 2.7% percent slopes, severely eroded FcC Fairview gravelly fine sandy 43.2 24.0% loam, 6 to 10 percent slopes FdE2 Fairview soils, 10 to 25 percent 47.8 26.5% slopes, moderately eroded TmC Tomlin loam, 6 to 10 percent 4.7 2.6% slopes Totals for Area of Interest 180.2 100.0% Map Unit Descriptions The map units delineated on the detailed soil maps in a soil survey represent the soils or miscellaneous areas in the survey area. The map unit descriptions, along with the maps, can be used to determine the composition and properties of a unit. A map unit delineation on a soil map represents an area dominated by one or more major kinds of soil or miscellaneous areas. A map unit is identified and named according to the taxonomic classification of the dominant soils. Within a taxonomic class there are precisely defined limits for the properties of the soils. On the landscape, however, the soils are natural phenomena, and they have the characteristic variability of all natural phenomena. Thus, the range of some observed properties may extend beyond the limits defined for a taxonomic class. Areas of soils of a single taxonomic class rarely, if ever, can be mapped without including areas of other taxonomic classes. Consequently, every map unit is made up of the soils or miscellaneous areas for which it is named and some minor components that belong to taxonomic classes other than those of the major soils. Most minor soils have properties similar to those of the dominant soil or soils in the map unit, and thus they do not affect use and management. These are called noncontrasting, or similar, components. They may or may not be mentioned in a particular map unit description. Other minor components, however, have properties 11 Custom Soil Resource Report and behavioral characteristics divergent enough to affect use or to require different management. These are called contrasting, or dissimilar, components. They generally are in small areas and could not be mapped separately because of the scale used. Some small areas of strongly contrasting soils or miscellaneous areas are identified by a special symbol on the maps. If included in the database for a given area, the contrasting minor components are identified in the map unit descriptions along with some characteristics of each. A few areas of minor components may not have been observed, and consequently they are not mentioned in the descriptions, especially where the pattern was so complex that it was impractical to make enough observations to identify all the soils and miscellaneous areas on the landscape. The presence of minor components in a map unit in no way diminishes the usefulness or accuracy of the data. The objective of mapping is not to delineate pure taxonomic classes but rather to separate the landscape into landforms or Iandform segments that have similar use and management requirements. The delineation of such segments on the map provides sufficient information for the development of resource plans. If intensive use of small areas is planned, however, onsite investigation is needed to define and locate the soils and miscellaneous areas. An identifying symbol precedes the map unit name in the map unit descriptions. Each description includes general facts about the unit and gives important soil properties and qualities. Soils that have profiles that are almost alike make up a soil series. Except for differences in texture of the surface layer, all the soils of a series have major horizons that are similar in composition, thickness, and arrangement. Soils of one series can differ in texture of the surface layer, slope, stoniness, salinity, degree of erosion, and other characteristics that affect their use. On the basis of such differences, a soil series is divided into soil phases. Most of the areas shown on the detailed soil maps are phases of soil series. The name of a soil phase commonly indicates a feature that affects use or management. For example, Alpha silt loam, 0 to 2 percent slopes, is a phase of the Alpha series. Some map units are made up of two or more major soils or miscellaneous areas. These map units are complexes, associations, or undifferentiated groups. A complex consists of two or more soils or miscellaneous areas in such an intricate pattern or in such small areas that they cannot be shown separately on the maps. The pattern and proportion of the soils or miscellaneous areas are somewhat similar in all areas. Alpha -Beta complex, 0 to 6 percent slopes, is an example. An association is made up of two or more geographically associated soils or miscellaneous areas that are shown as one unit on the maps. Because of present or anticipated uses of the map units in the survey area, it was not considered practical or necessary to map the soils or miscellaneous areas separately. The pattern and relative proportion of the soils or miscellaneous areas are somewhat similar. Alpha -Beta association, 0 to 2 percent slopes, is an example. An undifferentiated group is made up of two or more soils or miscellaneous areas that could be mapped individually but are mapped as one unit because similar interpretations can be made for use and management. The pattern and proportion of the soils or miscellaneous areas in a mapped area are not uniform. An area can be made up of only one of the major soils or miscellaneous areas, or it can be made up of all of them. Alpha and Beta soils, 0 to 2 percent slopes, is an example. 12 Custom Soil Resource Report Some surveys include miscellaneous areas. Such areas have little or no soil material and support little or no vegetation. Rock outcrop is an example. 13 Custom Soil Resource Report Catawba County, North Carolina U13—Clifford sandy loam, 2 to 6 percent slopes Map Unit Setting National map unit symbol: 2mlx4 Elevation: 200 to 2,000 feet Mean annual precipitation: 37 to 60 inches Mean annual air temperature: 50 to 59 degrees F Frost -free period: 160 to 200 days Farmland classification: All areas are prime farmland Map Unit Composition Clifford and similar soils: 90 percent Minor components: 3 percent Estimates are based on observations, descriptions, and transects of the mapunit. Description of Clifford Setting Landform: Interfluves Landform position (two-dimensional): Summit Landform position (three-dimensional): Interfluve Down -slope shape: Convex Across -slope shape: Convex Parent material: Saprolite derived from granite and gneiss and/or schist Typical profile Ap - 0 to 6 inches: sandy loam BA - 6 to 10 inches: sandy loam Bt - 10 to 47 inches: clay BC - 47 to 57 inches: clay loam CB - 57 to 80 inches: loam Properties and qualities Slope: 2 to 6 percent Depth to restrictive feature: More than 80 inches Drainage class: Well drained Runoff class: Low Capacity of the most limiting layer to transmit water (Ksat): Moderately high to high (0.57 to 1.98 in/hr) Depth to water table: More than 80 inches Frequency of flooding: None Frequency of ponding: None Available water supply, 0 to 60 inches: Moderate (about 8.3 inches) Interpretive groups Land capability classification (irrigated): None specified Land capability classification (nonirrigated): 2e Hydrologic Soil Group: A Ecological site: F136XY320VA - Mesic temperature regime, acidic upland forest, moist Hydric soil rating: No 14 Custom Soil Resource Report Minor Components Westfield Percent of map unit: 3 percent Landform: Interfluves Landform position (two-dimensional): Summit Landform position (three-dimensional): Interfluve Down -slope shape: Convex Across -slope shape: Convex Hydric soil rating: No M—Clifford sandy loam, 6 to 10 percent slopes Map Unit Setting National map unit symbol: 2mlx5 Elevation: 200 to 2,000 feet Mean annual precipitation: 37 to 60 inches Mean annual air temperature: 50 to 59 degrees F Frost -free period: 160 to 200 days Farmland classification: Farmland of statewide importance Map Unit Composition Clifford and similar soils: 90 percent Minor components: 4 percent Estimates are based on observations, descriptions, and transects of the mapunit. Description of Clifford Setting Landform: Interfluves Landform position (two-dimensional): Summit Landform position (three-dimensional): Interfluve Down -slope shape: Convex Across -slope shape: Convex Parent material: Saprolite derived from granite and gneiss and/or schist Typical profile Ap - 0 to 6 inches: sandy loam BA - 6 to 10 inches: sandy loam Bt - 10 to 47 inches: clay BC - 47 to 57 inches: clay loam CB - 57 to 80 inches: loam Properties and qualities Slope: 6 to 10 percent Depth to restrictive feature: More than 80 inches Drainage class: Well drained Runoff class: Medium Capacity of the most limiting layer to transmit water (Ksat): Moderately high to high (0.57 to 1.98 in/hr) 15 Custom Soil Resource Report Depth to water table: More than 80 inches Frequency of flooding: None Frequency of ponding: None Available water supply, 0 to 60 inches: Moderate (about 8.3 inches) Interpretive groups Land capability classification (irrigated): None specified Land capability classification (nonirrigated): 3e Hydrologic Soil Group: A Ecological site: F136XY320VA - Mesic temperature regime, acidic upland forest, moist Hydric soil rating: No Minor Components Westfield Percent of map unit: 3 percent Landform: Hillslopes on ridges Landform position (two-dimensional): Backslope Landform position (three-dimensional): Side slope Down -slope shape: Linear Across -slope shape: Convex Hydric soil rating: No Woolwine Percent of map unit: 1 percent Landform: Hillslopes on ridges Landform position (two-dimensional): Backslope Landform position (three-dimensional): Side slope Down -slope shape: Linear Across -slope shape: Convex Hydric soil rating: No CgB2—Clifford sandy clay loam, 2 to 6 percent slopes, moderately eroded Map Unit Setting National map unit symbol: 2tgcz Elevation: 660 to 1,310 feet Mean annual precipitation: 39 to 51 inches Mean annual air temperature: 57 to 59 degrees F Frost -free period: 190 to 230 days Farmland classification: All areas are prime farmland Map Unit Composition Clifford, moderately eroded, and similar soils: 90 percent Minor components: 10 percent Estimates are based on observations, descriptions, and transects of the mapunit. 16 Custom Soil Resource Report Description of Clifford, Moderately Eroded Setting Landform: Interfluves Landform position (two-dimensional): Summit Landform position (three-dimensional): Interfluve Down -slope shape: Convex Across -slope shape: Convex Parent material: Saprolite residuum weathered from schist and/or saprolite residuum weathered from gneiss Typical profile Ap - 0 to 6 inches: sandy clay loam Btl - 6 to 37 inches: clay Bt2 - 37 to 52 inches: clay loam C - 52 to 80 inches: clay loam Properties and qualities Slope: 2 to 6 percent Depth to restrictive feature: More than 80 inches Drainage class: Well drained Runoff class: Low Capacity of the most limiting layer to transmit water (Ksat): Moderately high to high (0.57 to 1.98 in/hr) Depth to water table: More than 80 inches Frequency of flooding: None Frequency of ponding: None Available water supply, 0 to 60 inches: Moderate (about 7.3 inches) Interpretive groups Land capability classification (irrigated): None specified Land capability classification (nonirrigated): 2e Hydrologic Soil Group: B Ecological site: F136XY320VA - Mesic temperature regime, acidic upland forest, moist Hydric soil rating: No Minor Components Woolwine, moderately eroded Percent of map unit: 5 percent Landform: Interfluves Landform position (two-dimensional): Summit Landform position (three-dimensional): Interfluve Down -slope shape: Convex Across -slope shape: Convex Hydric soil rating: No Westfield, moderately eroded Percent of map unit: 5 percent Landform: Interfluves Landform position (two-dimensional): Summit Landform position (three-dimensional): Interfluve Down -slope shape: Convex Across -slope shape: Convex Hydric soil rating: No 17 Custom Soil Resource Report CgU—Clifford sandy clay loam, 6 to 10 percent slopes, moderately eroded Map Unit Setting National map unit symbol: 2tgd 1 Elevation: 660 to 1,310 feet Mean annual precipitation: 39 to 51 inches Mean annual air temperature: 57 to 59 degrees F Frost -free period: 190 to 230 days Farmland classification: Farmland of statewide importance Map Unit Composition Clifford, moderately eroded, and similar soils: 85 percent Minor components: 15 percent Estimates are based on observations, descriptions, and transects of the mapunit. Description of Clifford, Moderately Eroded Setting Landform: Interfluves Landform position (two-dimensional): Summit, shoulder Landform position (three-dimensional): Interfluve Down -slope shape: Convex Across -slope shape: Convex Parent material: Saprolite residuum weathered from schist and/or saprolite residuum weathered from gneiss Typical profile Ap - 0 to 6 inches: sandy clay loam Btl - 6 to 37 inches: clay Bt2 - 37 to 52 inches: clay loam C - 52 to 80 inches: clay loam Properties and qualities Slope: 6 to 10 percent Depth to restrictive feature: More than 80 inches Drainage class: Well drained Runoff class: Medium Capacity of the most limiting layer to transmit water (Ksat): Moderately high to high (0.57 to 1.98 in/hr) Depth to water table: More than 80 inches Frequency of flooding: None Frequency of ponding: None Available water supply, 0 to 60 inches: Moderate (about 7.3 inches) Interpretive groups Land capability classification (irrigated): None specified Land capability classification (nonirrigated): 3e Hydrologic Soil Group: B 18 Custom Soil Resource Report Ecological site: F136XY320VA - Mesic temperature regime, acidic upland forest, moist Hydric soil rating: No Minor Components Westfield, moderately eroded Percent of map unit: 8 percent Landform: Interfluves Landform position (two-dimensional): Summit, shoulder Landform position (three-dimensional): Interfluve Down -slope shape: Convex Across -slope shape: Convex Hydric soil rating: No Woolwine, moderately eroded Percent of map unit: 7 percent Landform: Interfluves Landform position (two-dimensional): Summit, shoulder Landform position (three-dimensional): Interfluve Down -slope shape: Convex Across -slope shape: Convex Hydric soil rating: No CsA—Codorus loam, 0 to 2 percent slopes, frequently flooded Map Unit Setting National map unit symbol: 2mlxw Elevation: 200 to 1,560 feet Mean annual precipitation: 40 to 48 inches Mean annual air temperature: 50 to 59 degrees F Frost -free period: 160 to 200 days Farmland classification: Prime farmland if drained and either protected from flooding or not frequently flooded during the growing season Map Unit Composition Codorus and similar soils: 85 percent Minor components: 15 percent Estimates are based on observations, descriptions, and transects of the mapunit. Description of Codorus Setting Landform: Flood plains Landform position (three-dimensional): Tread Down -slope shape: Concave Across -slope shape: Linear Parent material: Loamy alluvium derived from igneous and metamorphic rock Typical profile A - 0 to 8 inches: loam 19 Custom Soil Resource Report Bw1 - 8 to 18 inches: silty clay loam Bw2 - 18 to 30 inches: loam Bw3 - 30 to 38 inches: silt loam BCg - 38 to 50 inches: silt loam Cg - 50 to 80 inches: silt loam Properties and qualities Slope: 0 to 2 percent Depth to restrictive feature: More than 80 inches Drainage class: Somewhat poorly drained Runoff class: Low Capacity of the most limiting layer to transmit water (Ksat): Moderately high to high (0.57 to 1.98 in/hr) Depth to water table: About 6 to 24 inches Frequency of flooding: Frequent Frequency of ponding: None Available water supply, 0 to 60 inches: High (about 10.7 inches) Interpretive groups Land capability classification (irrigated): None specified Land capability classification (nonirrigated): 4w Hydrologic Soil Group: B/D Ecological site: F136XY11 OVA - Mesic temperature regime, flood plain forest, wet Hydric soil rating: No Minor Components Hatboro, undrained Percent of map unit: 5 percent Landform: Depressions on flood plains Landform position (three-dimensional): Tread Down -slope shape: Concave Across -slope shape: Linear Hydric soil rating: Yes Pfafftown Percent of map unit: 2 percent Landform: Stream terraces Landform position (three-dimensional): Tread Down -slope shape: Convex Across -slope shape: Linear Hydric soil rating: No Ronda Percent of map unit: 2 percent Landform: Natural levees on flood plains Landform position (three-dimensional): Tread Down -slope shape: Convex Across -slope shape: Convex Hydric soil rating: No Banister Percent of map unit: 2 percent Landform: Flats on stream terraces Landform position (three-dimensional): Tread Down -slope shape: Concave Across -slope shape: Linear 20 Custom Soil Resource Report Hydric soil rating: No Comus Percent of map unit: 2 percent Landform: Flood plains Landform position (three-dimensional): Tread Down -slope shape: Convex Across -slope shape: Linear Hydric soil rating: No Dan river Percent of map unit: 2 percent Landform: Flood plains Landform position (three-dimensional): Tread Down -slope shape: Convex Across -slope shape: Linear Hydric soil rating: No FaE3—Fairview clay loam, 10 to 25 percent slopes, severely eroded Map Unit Setting National map unit symbol: 2mlxr Elevation: 200 to 1,400 feet Mean annual precipitation: 37 to 60 inches Mean annual air temperature: 50 to 59 degrees F Frost -free period: 160 to 190 days Farmland classification: Not prime farmland Map Unit Composition Fairview, severely eroded, and similar soils: 85 percent Estimates are based on observations, descriptions, and transects of the mapunit. Description of Fairview, Severely Eroded Setting Landform: Hillslopes on ridges Landform position (two-dimensional): Backslope Landform position (three-dimensional): Side slope Down -slope shape: Linear Across -slope shape: Convex Parent material: Saprolite derived from granite and gneiss and/or schist Typical profile A - 0 to 3 inches: clay loam Bt - 3 to 29 inches: clay BC - 29 to 37 inches: clay loam C1 - 37 to 52 inches: clay loam C2 - 52 to 80 inches: loam Properties and qualities Slope: 10 to 25 percent 21 Custom Soil Resource Report Depth to restrictive feature: More than 80 inches Drainage class: Well drained Runoff class: Medium Capacity of the most limiting layer to transmit water (Ksat): Moderately high to high (0.57 to 1.98 in/hr) Depth to water table: More than 80 inches Frequency of flooding: None Frequency of ponding: None Available water supply, 0 to 60 inches: Moderate (about 7.7 inches) Interpretive groups Land capability classification (irrigated): None specified Land capability classification (nonirrigated): 6e Hydrologic Soil Group: B Ecological site: F136XY320VA - Mesic temperature regime, acidic upland forest, moist Hydric soil rating: No FcC—Fairview gravelly fine sandy loam, 6 to 10 percent slopes Map Unit Setting National map unit symbol: 2mm3b Elevation: 200 to 1,400 feet Mean annual precipitation: 40 to 48 inches Mean annual air temperature: 50 to 59 degrees F Frost -free period: 160 to 190 days Farmland classification: Farmland of statewide importance Map Unit Composition Fairview and similar soils: 85 percent Estimates are based on observations, descriptions, and transects of the mapunit. Description of Fairview Setting Landform: Hillslopes on ridges Landform position (two-dimensional): Backslope Landform position (three-dimensional): Side slope Down -slope shape: Linear Across -slope shape: Convex Parent material: Saprolite derived from granite and gneiss and/or schist Typical profile A - 0 to 3 inches: gravelly fine sandy loam E - 3 to 7 inches: gravelly fine sandy loam Bt - 7 to 25 inches: sandy clay C - 25 to 80 inches: sandy clay loam Properties and qualities Slope: 6 to 10 percent Depth to restrictive feature: More than 80 inches Drainage class: Well drained 22 Custom Soil Resource Report Runoff class: Medium Capacity of the most limiting layer to transmit water (Ksat): Moderately high to high (0.57 to 1.98 in/hr) Depth to water table: More than 80 inches Frequency of flooding: None Frequency of ponding: None Available water supply, 0 to 60 inches: Moderate (about 7.3 inches) Interpretive groups Land capability classification (irrigated): None specified Land capability classification (nonirrigated): 3e Hydrologic Soil Group: B Ecological site: F136XY320VA - Mesic temperature regime, acidic upland forest, moist Hydric soil rating: No FdE2—Fairview soils, 10 to 25 percent slopes, moderately eroded Map Unit Setting National map unit symbol: 2mm2s Elevation: 200 to 3,500 feet Mean annual precipitation: 40 to 65 inches Mean annual air temperature: 50 to 59 degrees F Frost -free period: 160 to 200 days Farmland classification: Not prime farmland Map Unit Composition Fairview, moderately eroded, and similar soils: 75 percent Minor components: 10 percent Estimates are based on observations, descriptions, and transects of the mapunit. Description of Fairview, Moderately Eroded Setting Landform: Hillslopes on ridges Landform position (two-dimensional): Backslope Landform position (three-dimensional): Side slope Down -slope shape: Linear Across -slope shape: Convex Parent material: Saprolite derived from schist and/or gneiss Typical profile Ap - 0 to 9 inches: sandy clay loam Bt - 9 to 24 inches: clay BCt - 24 to 29 inches: sandy clay loam C - 29 to 80 inches: loam Properties and qualities Slope: 10 to 25 percent Depth to restrictive feature: More than 80 inches Drainage class: Well drained Runoff class: High 23 Custom Soil Resource Report Capacity of the most limiting layer to transmit water (Ksat): Moderately high to high (0.57 to 1.98 in/hr) Depth to water table: More than 80 inches Frequency of flooding: None Frequency of ponding: None Available water supply, 0 to 60 inches: Moderate (about 8.3 inches) Interpretive groups Land capability classification (irrigated): None specified Land capability classification (nonirrigated): 4e Hydrologic Soil Group: B Ecological site: F136XY320VA - Mesic temperature regime, acidic upland forest, moist Hydric soil rating: No Minor Components Meadowfield Percent of map unit: 5 percent Landform: Hillslopes on ridges Landform position (two-dimensional): Backslope Landform position (three-dimensional): Side slope Down -slope shape: Linear Across -slope shape: Convex Hydric soil rating: No Woolwine, moderately eroded Percent of map unit: 5 percent Landform: Hillslopes on ridges Landform position (two-dimensional): Backslope Landform position (three-dimensional): Side slope Down -slope shape: Linear Across -slope shape: Convex Hydric soil rating: No TmC—Tomlin loam, 6 to 10 percent slopes Map Unit Setting National map unit symbol: 2mm27 Elevation: 200 to 1,400 feet Mean annual precipitation: 37 to 60 inches Mean annual air temperature: 50 to 59 degrees F Frost -free period: 160 to 190 days Farmland classification: Farmland of statewide importance Map Unit Composition Tomlin and similar soils: 90 percent Estimates are based on observations, descriptions, and transects of the mapunit. 24 Custom Soil Resource Report Description of Tomlin Setting Landform: Hillslopes on ridges Landform position (two-dimensional): Backslope Landform position (three-dimensional): Side slope Down -slope shape: Linear Across -slope shape: Convex Parent material: Saprolite derived from diorite and/or gabbro and/or diabase and/or gneiss Typical profile Apt - 0 to 4 inches: loam Ap2 - 4 to 8 inches: clay loam Bt1 - 8 to 30 inches: clay Bt2 - 30 to 37 inches: silty clay Bt3 - 37 to 49 inches: silty clay loam BCt - 49 to 57 inches: silt loam C - 57 to 81 inches: loam Properties and qualities Slope: 6 to 10 percent Depth to restrictive feature: More than 80 inches Drainage class: Well drained Runoff class: Medium Capacity of the most limiting layer to transmit water (Ksat): Moderately high to high (0.57 to 1.98 in/hr) Depth to water table: More than 80 inches Frequency of flooding: None Frequency of ponding: None Sodium adsorption ratio, maximum: 1.0 Available water supply, 0 to 60 inches: Moderate (about 8.2 inches) Interpretive groups Land capability classification (irrigated): None specified Land capability classification (nonirrigated): 3e Hydrologic Soil Group: B Ecological site: F136XY320VA - Mesic temperature regime, acidic upland forest, moist Hydric soil rating: No 25 References American Association of State Highway and Transportation Officials (AASHTO). 2004. Standard specifications for transportation materials and methods of sampling and testing. 24th edition. American Society for Testing and Materials (ASTM). 2005. Standard classification of soils for engineering purposes. ASTM Standard D2487-00. Cowardin, L.M., V. Carter, F.C. Golet, and E.T. LaRoe. 1979. Classification of wetlands and deep -water habitats of the United States. U.S. Fish and Wildlife Service FWS/OBS-79/31. Federal Register. July 13, 1994. Changes in hydric soils of the United States. Federal Register. September 18, 2002. Hydric soils of the United States. Hurt, G.W., and L.M. Vasilas, editors. Version 6.0, 2006. Field indicators of hydric soils in the United States. National Research Council. 1995. Wetlands: Characteristics and boundaries. Soil Survey Division Staff. 1993. Soil survey manual. Soil Conservation Service. U.S. Department of Agriculture Handbook 18. http://www.nres.usda.gov/wps/portal/ nres/detail/national/soils/?cid=nres 142p2_054262 Soil Survey Staff. 1999. Soil taxonomy: A basic system of soil classification for making and interpreting soil surveys. 2nd edition. Natural Resources Conservation Service, U.S. Department of Agriculture Handbook 436. http:// www.nres.usda.gov/wps/portal/nres/detail/national/soils/?cid=nres142p2_053577 Soil Survey Staff. 2010. Keys to soil taxonomy. 11th edition. U.S. Department of Agriculture, Natural Resources Conservation Service. http:// www. nres.usda.gov/wps/portal/nres/detail/national/soils/?cid=nres142p2_053580 Tiner, R.W., Jr. 1985. Wetlands of Delaware. U.S. Fish and Wildlife Service and Delaware Department of Natural Resources and Environmental Control, Wetlands Section. United States Army Corps of Engineers, Environmental Laboratory. 1987. Corps of Engineers wetlands delineation manual. Waterways Experiment Station Technical Report Y-87-1. United States Department of Agriculture, Natural Resources Conservation Service. National forestry manual. http://www.nres.usda.gov/wps/portal/nres/detail/soils/ home/?cid=nres142p2_053374 United States Department of Agriculture, Natural Resources Conservation Service. National range and pasture handbook. http://www.nres.usda.gov/wps/portal/nres/ detail/national/landuse/rangepasture/?cid=stelprdb1043084 26 Custom Soil Resource Report United States Department of Agriculture, Natural Resources Conservation Service. National soil survey handbook, title 430-VI. http://www.nres.usda.gov/wps/portal/ nres/detail/soils/scientists/?cid=nres142p2_054242 United States Department of Agriculture, Natural Resources Conservation Service. 2006. Land resource regions and major land resource areas of the United States, the Caribbean, and the Pacific Basin. U.S. Department of Agriculture Handbook 296. http://www.nres.usda.gov/wps/portal/nres/detail/national/soils/? cid=nres142p2_053624 United States Department of Agriculture, Soil Conservation Service. 1961. Land capability classification. U.S. Department of Agriculture Handbook 210. http:// www.nrcs.usda.gov/lnternet/FSE—DOCUMENTS/nrcsl 42p2_052290.pdf 27 Eastern Band of Cherokee Indians I Cherokee Trout Hatc Civil Calculations ��� Appendices Appendix B — NOAA Rainfall Data NOAA Atlas 14, Volume 2, Version 3 ' Location name: Hickory, North Carolina, USA*�' Latitude: 35.7215°, Longitude:-81.3103° Elevation: 1063 ft** source: ESRI Maps ** source: USGS`" POINT PRECIPITATION FREQUENCY ESTIMATES G.M. Bonnin, D. Martin, B. Lin, T. Parzybok, M.Yekta, and D. Riley NOAA, National Weather Service, Silver Spring, Maryland PF tabular I PF graphical I Maps & aerials PF tabular 11 PDS-based point precipitation freciuencv estimates with 90% confidence intervals (in inches/hour)1 11 Average recurrence interval (years) Duration ����� 1 2 5 10 25 50 100 200 5-min 4.43 5.24 6.19 6- 7.82 8.48 9.14 9.79 (4.07-4.82) (4.82-5.71) 1 (5.68-6.76) 1 (6.31-7.54) (7.08-8.53) (7.63-9.28) 1 (8.15-10.0) 1 (8.63-10.8) 10-min 3.53 4.19 4.96 5.53 6.23 6.76 7.27 7.76 (3.25-3.85) 1 (3.86-4.57) 11 (4.54-5.41) 1 (5.05-6.02) (5.65-6.80) (6.07-7.39) 1 (6.47-7.97) 15-min 2.94 3.51 4.18 4.66 5.26 5.70 6.12 6.53 (2.71-3.21) 1 (3.23-3.83) 1 (3.83-4.56) 1 (4.26-5.08) 1 (4.77-5.74) 1 (5.13-6.23) 1 (5.46-6.72) 1 (5.75-7.20) 30-min 2.02 2.43 2.97 3.38 3.90 4.29 4.69 5.08 (1.86-2.20) 1 (2.23-2.65) 1 (2.72-3.24) 1 (3.08-3.68) 1 (3.53-4.26) 1 (3.86-4.69) 1 (4.18-5.15) 1 (4.47-5.61) 60-min 1.26 1.52 1.90 2.20 2.60 2.91 3.23 3.56 (1.16-1.37) 1 (1.40-1.66) 1 (1.74-2.08) 1 (2.01-2.40) 1 (2.35-2.83) 1 (2.62-3.18) 1 (2.88-3.54) (3.14-3.93) 2-hr 0.732 0.889 1.12 1.31 1.56 1.77 1.99 2.22 (0.671-0.798) (0.814-0.971) (1.03-1.23) 1 (1.19-1.43) 1 (1.41-1.71) 1 (1.58-1.94) 1 (1.76-2.19) 3-hr 0.522 0.632 0.800 0.934 1.12 1.28 1.45 1.62 (0.479-0.574) (0.579-0.695) (0.730-0.879) (0.849-1.02) 1 (1.01-1.24) 1 (1.14-1.41) 11 (1.28-1.60) (1.42-1.81) 6-hr 0.324 0.390 0.491 0.572 0.687 0.782 0.882 0.989 (0.298-0.354) (0.359-0.427) (0.450-0.537) (0.522-0.625) (0.622-0.750) (0.702-0.856) (0.783-0.969) (0.868-1.09) 500 1000 10.6 11.3 (9.19-11.8) (9.60-12 8.39 F 8.86 (7.27-9.34) (7.55-9.f 7.04 T 7.42 (6.10-7.84) (6.32-8. 5.60 6.00 (4.85-6.24) 1 (5.12-6.7 4.02 4.38 2.54 11 2.80 (2.18-2.84) 11 (2.36-3.16) 1.88 2.09 (1.60-2.12) 11 (1.76-2.37) 1.14 1.27 (0.982-1.27) (1.07-1.42) 0.198 0.239 0.300 0.348 0.415 0.470 0.527 0.586 0.670 0.738 12-hr (0.183-0.216) (0.221-0.261) (0.276-0.327) (0.319-0.379) (0.378-0.452) (0.424-0.512) (0.471-0.575) (0.518-0.642) (0.583-0.737) (0.633-0.815) 0.150 0.190 0.221 0.265 0.299 0.335 0.372 0.423 0.463 Ej��E]F-0.-123 (0.115-0.134) (0.139-0.162) (0.176-0.206) (0.204-0.240) (0.2. 3-0.287) (0.274-0.324) (0.305-0.363) (0.337-0.404) (0.381-0.460) (0.415-0.505) 2-day 0.073 11 0.089 11 0.111 11 0.129 0.153 11 0.172 1 0.191 0.211 11 0.238 0.260 (0.068-0.080) (0.082-0.096) (0.103-0.121) (0.119-0.140) (0.141-0.166) (0.157-0.187) (0.175-0.208) (0.192-0.230) (0.215-0.259) (0.233-0.283) 3-day 0.052 0.063 0.078 0.090 0.107 0.120 0.133 0.146 0.165 0.179 (0.048-0.056) (0.058-0.068) (0.072-0.085) (0.083-0.098) (0.098-0.115) (0.110-0.129) (0.121-0.144) (0.133-0.159) (0.149-0.179) (0.161-0.195) 4-day 0.041 0.049 0.062 0.071 0.084 0.093 0.104 0.114 0.128 0.139 (0.038-0.044) (0.046-0.053) (0.057-0.066) (0.065-0.076) (0.077-0.090) (0.086-0.101) (0.095-0.112) (0.104-0.123) (0.116-0.139) (0.126-0.151) 7-day 0.027 0.032 0.039 0.045 0.052 0.058 0.064 0.069 0.077 0.083 (0.025-0.029) (0.030-0.035) (0.037-0.042) (0.042-0.048) (0.048-0.056) (0.054-0.062) (0.059-0.068) (0.064-0.075) (0.071-0.083) (0.076-0.090) 10-day 0.021 0.026 0.031 0.035 0.040 0.044 0.048 0.052 0.058 0.062 (0.020-0.023) (0.024-0.027) (0.029-0.033) (0.033-0.037) (0.037-0.043) (0.041-0.047) (0.045-0.052) (0.048-0.056) (0.053-0.062) (0.057-0.066) 20-day 0.014 0.017 0.020 0.022 0.026 0.028 6.031 0.033 6.036 0.039 (0.013-0.015) (0.016-0.018) (0.019-0.021) (0.021-0.024) (0.024-0.027) (0.026-0.030) (0.029-0.032) (0.031-0.035) (0.034-0.039) (0.036-0.041) 30-day 0.012 0.014 0.016 0.017 T 0.019 0.021 0.022 F 0.024 0.026 0.027 (0.011-0.012) (0.013-0.014) (0.015-0.017) (0.017-0.018) (0.018-0.020) (0.020-0.022) (0.021-0.024) (0.023-0.025) (0.024-0.027) (0.025-0.029) 45-day 0.010 0.011 0.013 0.014 0.016 0.017 0.018 0.019 0.020 0.021 (0.009-0.010) (0.011-0.012) (0.012-0.014) (0.013-0.015) (0.015-0.016) (0.016-0.017) (0.017-0.018) (0.018-0.019) (0.019-0.021) (0.020-0.022) 60-day 0.009 0.010 0.011 0.012 0.013 0.014 0.015 0.016 0.017 0.018 (0.008-0.009) (0.010-0.010) (0.011-0.012) (0.012-0.013) (0.013-0.014) (0.014-0.015) (0.015-0.016) (0.015-0.017) (0.016-0.018) (0.017-0.019) t Precipitation frequency (PF) estimates in this table are based on frequency analysis of partial duration series (PDS). umbers in parenthesis are PF estimates at lower and upper bounds of the 90% confidence interval. The probability that precipitation frequency estimates (for given duration and average recurrence interval) will be greater than the upper bound (or less than the lower bound) is 5%. Estimates at upper bounds are not iecked against probable maximum precipitation (PMP) estimates and may be higher than currently valid PMP values. refer to NOAAAtlas 14 document for more information. Back to Top PF graphical PD5-based intensity -duration -frequency (IDF) curves Latitude: 35.7215', Longitude_-81.3103' 101 c L- >. :�, >. }, >, 7, 7. >, � -cp b 4 U b Lf5 O u'i O O n N N r~ O N rr5 1D m La Duration' 101 10 -2 NOAAAtlas 14, Volume 2, Versian 3 4 4 i4 4i ii i Average recurrence interval (years) Created (GMT}_ Man Noy 27 15:02.09 202 3 Back to Top Maps & aerials Small scale terrain Average recurrence interval tyeara} — 1 2 — s — 10 25 — so 100 200 •— goo 1000 Duration — 5-mn — 2-day — IO-min — 3-day 15-rnln — 4-day — 30-min — 7-day — 60-min — 10-day — 2-hr 20-day — 3-hr — 30-day — "ir — 45-day — 12-hr — 5 D-day 24-hr jw angvi ff II Hickory 1, Large scale terrain FIT- _ Ki 1195port BI Istol J011115011 6ty" Winston-Salem 4P • Dul Greensboro jk "Ashedille FORTH C A R 0 L I N A Charlotte ter I 00k 4MI T T n N T T WT A Large scale map Bri5fo fem Greensborc A h -11 k!�w; e2 North Carolina in-flOtte on _S t\ North Carolina Fitte 100km 60mi Large scale aerial Back to Top US Department of Commerce National Oceanic and Atmospheric Administration National Weather Service National Water Center 1325 East West Highway Silver Spring, MD 20910 Questions?: HDSC.Questions noaa.gov Disclaimer NOAA Atlas 14, Volume 2, Version 3 ' Location name: Hickory, North Carolina, USA ", Latitude: 35.721*, Longitude:-81.3103° Elevation: 1085 ft** source: ESRI Maps ** source: USGS`" POINT PRECIPITATION FREQUENCY ESTIMATES G.M. Bonnin, D. Martin, B. Lin, T. Parzybok, M.Yekta, and D. Riley NOAA, National Weather Service, Silver Spring, Maryland PF tabular I PF graphical I Maps & aerials PF tabular PDS-based point precipitation frequency estimates with 90% confidence intervals (in inches)' Average recurrence interval (years) Duration ���� 1 2 5 10 25 50 100 200 500 1000 0.369 0.437 0.516 0.576 0.652 0.707 0.762 0.816 0.884 0.938 5-min (0.339-0.402) (0.402-0.476) (0.473-0.563) (0.526-0.628) (0.590-0.711) (0.636-0.773) (0.679-0.836) (0.719-0.901) (0.766-0.985) (0.800-1.05) 0.589 0.699 0.826 0.922 1.04 1.13 1.21 1.29 1.40 1.48 10-min (0.542-0.642) (0.643-0.762) (0.757-0.901) (0.841-1.00) (0.941-1.13) 1 (1.01-1.23) 1 (1.08-1.33) 1 (1.14-1.43) 1 (1.21-1.56) (1.26-1.66) 0.736 0.878 1.04 1.17 1.32 1.42 1.53 1.63 1.76 1.85 15-min (0.677-0.802) (0.808-0.958) (0.958-1.14) 1 (1.06-1.27) 11 (1.19-1.44) 1 (1.28-1.56) 1 (1.36-1.68) 11 (1.44-1.80) 1 (1.52-1.96) (1.58-2.08) 1.01 1.21 1.48 1.69 1.95 2.15 2.34 2.54 2.80 3.00 30-min (0.929-1.10) 1 (1.12-1.32) 11 (1.36-1.62) 1 (1.54-1.84) 11 (1.77-2.13) 1 (1.93-2.35) 1 (2.09-2.57) 11 (2.24-2.80) 1 (2.43-3.12) (2.56-3.37) 1.26 1.52 1.90 2.20 2.60 2.91 3.23 3.56 4.02 4.38 60-min (1.16-1.37) 1 (1.40-1.66) 11 (1.74-2.08) 1 (2.01-2.40) 11 (2.35-2.83) 1 (2.62-3.18) (2.88-3.54) (3.14-3.93) (3.48-4.48) (3.74-4.92) 2-hr 1.46 1.78 2.25 2.62 3.13 3.54 3.98 4.43 5.08 5.60 (1.34-1.60) (1.63-1.94) 11 (2.05-2.46) (2.38-2.86) (2.83-3.42) (3.17-3.88) (3.52-4.38) (3.88-4.91) (4.36-5.67) (4.73-6.31) 1.57 1.90 2.40 2.81 3.38 3.85 4.35 4.88 5.65 6.28 3-hr (1.44-1.72) (1.74-2.09) 1 (2.20-2.64) (2.55-3.08) (3.04-3.71) (3.44-4.25) (3.84-4.81) 1 (4.26-5.44) (4.82-6.35) (5.28-7.13) 1.94 2.34 2.94 3.43 4.12 4.68 5.28 5.92 6.84 7.59 6-hr (1.79-2.12) (2.15-2.56) (2.70-3.22) (3.13-3.74) (3.73-4.50) (4.21-5.13) (4.69-5.81) 1 (5.20-6.55) (5.88-7.62) (6.42-8.52) 2.39 2.89 3.62 4.20 5.01 5.67 6.35 7.07 8.08 8.89 12-hr (2.21-2.60) (2.66-3.15) (3.33-3.94) (3.85-4.57) (4.56-5.45) (5.12-6.17) (5.68(5.68-6.93) 11 (6.25-7.74) (7.04-8.88) (7.64-9.82) 24-hr 2.97 3.60 4.57 5.32 6.36 7.20 8.05 8.94 10.2 11.1 ) (2.76-3.22) (3.34-3.91) (4.22-4.96) (4.91-5.77) (5.85-6.89) (6.59-7.80) (7.34-8.73) (8.10-9.71) (9.14-11.1) (9.97-12.1 2-day 428 5.38 6.22 7.38 8.29 10.2 11.5 12.53.54 . (3.28-3.84) 1 (3.96-4.65) 11 (4.97-5.83) 1 (5.74-6.74) (6.78-8.00) (7.58-8.99) (8.40-10.0) (9.23-11.1) 1 (10.4-12.5) 1 (11.2-13.6) 3.77 4.54 5.66 6.54 7.72 8.66 9.60 10.6 11.9 12.9 3-day (3.49-4.07) (4.21-4.91) (5.24-6.12) (6.03-7.06) (7.10-8.34) (7.93-9.36) (8.77-10.4) (9.62-11.5 10.8-12.9 11.7-14.1 ) ( ) ( ) 3.99 4.80 5.95 6.85 8.07 9.02 9.99 11.0 12.3 13.4 4-day (3.70-4.29) 1 (4.45-5.17) 1 (5.52-6.42) (6.33-7.38) (7.43-8.69) (8.28-9.73) (9.13-10.8) 1 (10.0-11.9) 1 (11.2-13.4) (12.1-14.5) 4.60 5.51 6.71 7.64 F 8.86 F 9.82 10.8 11.8 13.1 14.1 7-day ( 10.8-12.6) (12.0-14.1) ( 12.8-15.2) (4 .30-4.93) (5.14-5.90) (6.26-7.20) (7.11-8.19) (8.23-9.51) (9.09-10.5) (9.95-11.6) 11 5.27 6.28 7.55 8.51 9.77 10.7 11.7 12.7 14.0 15.0 10-day (4.95-5.62) (5.89-6.70) (7.08-8.05) 1 (7.96-9.07) (9.12-10.4) (10.0-11.5) 1 (10.9-12.5) 1 1 (12.9-15.0) (13.7-16.0) 7.03 8.32 F 9.83 11.0 12.5 13.7 14.9 16.1 17.7 18.9 20-day (6.64-7.45) (7.85-8.82) (9.26-10.4) (10.3-11.6) (11.8-13.3) (12.9-14.5) 1 (13.9-15.8) 11 (15.0-17.1) 1 (16.4-18.8) (17.5-20.1) 30-day 8.69 10.2 11.8 12.9 14.4 15.5 16.5 17.6 18.9 19.9 (8.29-9.12) (9.74-10.7) (11.2-12.4) (12.3-13.6) (13.7-15.1) (14.7-16.3) (15.7-17.4) (16.6-18.5) (17.8-19.9) (18.7-21.0) 11.0 12.8 14.5 15.7 17.3 18.4 19.5 F 20.6 22.0 23.0 45-day (10.5-11.5) 1 (12.3-13.4) 11 (13.9-15.2) 1 (15.0-16.4) (16.5-18.1) (17.6-19.3) 1 (18.6-20.5) 1 (19.6-21.6) 1 (20.9-23.0) (21.8-24.1) 60-day 13.0 15.2 17.0 18.4 20.2 21.4 22.7 23.9 25.4 26.5 (12.5-13.6) (14.6-15.8) (16.3-17.8) (17.7-19.2) (19.3-21.0) (20.5-22.4) (21.7-23.7) (22.8-24.9) (24.2-26.6) (25.2-27.8) 1 Precipitation frequency (PF) estimates in this table are based on frequency analysis of partial duration series (PDS). Numbers in parenthesis are PF estimates at lower and upper bounds of the 90% confidence interval. The probability that precipitation frequency estimates (for a given duration and average recurrence interval) will be greater than the upper bound (or less than the lower bound) is 5%. Estimates at upper bounds are not checked against probable maximum precipitation (PMP) estimates and may be higher than currently valid PMP values. Please refer to NOAA Atlas 14 document for more information. Back to Top PF graphical 25 E 20 Ld a 5 t:u PD5-based depth -duration -frequency {DDF) curves Latitude: 35.7214', Longitude_-81.31031 c e e_ c c_ 6- L a, Z�, >. }, >, 7, 7 >, �', L L N f�7 4� CV -cp b 4 -0 b n N N r~ cS N rr5 1D m La Duration' 25 - C 20 - 10 2 a 5 M NOAAAtlas 14, Volume 2, Versian 3 p 0 F, 4 4 i4 4i ii r Average recurrence interval (years) ic Created (GMT}_ Man Noy 77 17.17.54 202� Back to Top Maps & aerials Small scale terrain Average recurrence interval tyeara} — 1 2 — 5 — 10 25 so 100 200 •— 600 1000 Duration — 5-mn — 2-day — 14-min — 3-day 15-rnln — 4-day — 3"in — 7-d ay — 60-min — 10-day — 2-hr 20-day — 3-hr — 30-day — "ir — 45-day — 12-hr — 5 D-day 24-hr ongvi 2mi M, Large scale terrain %V Kingsport' BI Stol J011115011 city" Winston-Salem �ti • Dul Greensboro jkI FORTH C A R 0 L I N A Charlotte ter I 00k 4MI T T n N T T WT A Large scale map Bri5fo --ff Greensborc A h -11 k!�w; e2 North Carolina in-flOtte North Carolina rl tte 100km 60mi Large scale aerial Back to Top US Department of Commerce National Oceanic and Atmospheric Administration National Weather Service National Water Center 1325 East West Highway Silver Spring, MD 20910 Questions?: HDSC.Questions noaa.gov Disclaimer Eastern Band of Cherokee Indians I Cherokee Trout Hatc Civil Calculations ��� Appendices Appendix C — Drainage Area Maps 1 04 7N\ 9 ��� --�r o 'ri-j �%' .,.r:f-yj�'-� \ .� /p ?.% � i' ,,.. .��C � 1� l \ .` 1 a'�d t; �1,�`:�� � r\ � � .� ��-�'� �. / 4ro, It --rr .2m il/• 1J `\ .,J �) �ii/�/ -�r / 4� '�S �, .s ��- Ja _ ,Q ,�y�q�L� J-C - i ,ll -` , .t!)' 3 \1 tl \ _� . 00 / � � / � f�-� � �-' � 10: e !� �'� -ram._ `,• \V' . ��. U// r 1 �'- J �=J �V / /�`�.�" �. 1� �. "r O ,••1 ` r Ob \ \ C 7/ C. 6p S( 'Wove A5 - �o � � � � < �)) / ��i fir/ � ;. �,,��: � r � � -� � ' � \ `�' --� , �,;. - f :� . -j N-, C9 43 FcIE2�-IFAIF�VIEW SOIL SOIL GROUP: B 10 aN, o� -� CfB- CLIFFORD SANDY LOAM SOIL GR_ _ OUP: A 47- 01, F, FcC-FAIRVIEW GRAVELLY FINE SANDY LOAM SOIL GROUP: B LEGEND ` YJ: \`�� \ `J� 1/ i //11� r/y(/I \� \ � .ram.-.. ✓ �_� ... �� � � `��-'� �/ � •1 I s ram/ J look! WATERSHED BOUNDARY TOC PATH PROPOSED CULVERT EXISTING CONTOUR SOIL MAP FEMA FLOODPLAIN r A� - Eastern Band of Cherokee Indians I Cherokee Trout Hatc Civil Calculations ��� Appendices Appendix D — Stormwater Peak Flow Calculations Composite S lm:)M� Curve Numberer PROJECT: Duke Energy Sweetwater Tap Relocation DATE: 11/22/2023 SCENARIO: PREPARED BY: CJS Drainage Area: Culvert Total Drainage Area: 38.00 Ac Hydrologic Soil Group A B C D Area Area Area Area Cover Description Ac 1 CN Ac CN Ac 1 CN Ac 1 CN Onen snace (lawns. narks. aolf courses. cemeteries. etc-1- Poor condition (grass cover < 50%) Fair condition(grass cover 50% to 75% 8.92 1 49 10.22 1 69 & Good condition (grass cover > 75%) 1 39 1 61 80 llmnarvinus areas• I I I I Paved parking lots, roofs, driveways, etc. (excluding R/W) 1 98 98 98 Paved streets and roads; curbs and storm sewers(excluding right 11.10 1 98 98 98 Paved streets and roads; open ditches (including R/W) 83 89 93 Gravel streets and roads (including R/W) 76 85 91 Dirt streets and roads (including R/W) 72 1 82 89 Western desert urban areas: Natural desert landscaping (pervious areas only) 63 77 88 Artificial desert landscaping (impervious weed barrier, desert 96 96 96 Urban districts: Commercial and business 89 92 11 94 95 Industrial 81 88 91 93 Residential districts by average lot size: 1/8 acre or less (town houses) 77 85 90 92 1/4 acre 61 75 83 87 1/3 acre 57 72 81 86 1/2 acre 54 70 80 85 1 acre 51 68 79 84 2 acres 46 65 77 82 Pasture, grassland or range: Poor hydrologic condition 68 11 79 86 89 Fair hydrologic condition 49 69 79 84 Good hydrologic condition 39 61 74 80 Woods: Poor hydrologic condition 45 i 66 77 83 Fair hydrologic condition 3.65 1 36 1 4.11 1 60 1 73 1 79 Good hydrologic condition 30 55 1 70 77 Cultivated Agricultural Areas: Fallow Bare Soil Crop residue Cover Good Hydrolic Condition 83 i 88 i 90 Developing urban areas: Newly graded areas (pervious areas only, no vegetation) 86 91 94 Total HSG Areas: 1 23.67 14.33 Calculated Total Drainage Area: 38.00 Ac Calculated Composite Curve Number: 69 12/18/2023 Time of Concentration Worksheet F:)R SCS TR-55 Method PROJECT: Sweetwater tap relocation DATE: 11/22/23 SCENARIO: Post -Developed Conditions PREPARED BY: Clarke Summers Drainage Area Information Drainage Area Tc Summary Data DRAINAGE AREA ID: Flow Type Length (ft) Elev. Diff. Tc TOTAL BASIN LENGTH: 1720.4 ft Sheet Flow 100.0 4.00 13.2 mins. TOTAL ELEVATION UP: 1158.60 Shallow Concentrated Flow 1620.4 116.70 6.2 mins. TOTAL ELEVATION DOWN: 1037.90 Channel Flow - Rectangular 0.0 0.00 0.0 mins. TOTAL ACRES: 38.00 Channel Flow - Triangular 0.0 0.00 0.0 mins. Channel Flow - Trapezoidal 0.0 0.00 0.0 mins. Channel Flow - Circular 0.0 0.00 0.0 mins. Basin Totals1720.4 120.7019.4 mins. This time of concentration calculation is based on survey data, aerial photography, and field investigation. 1. SHEET FLOW M 0 2. SHALLOW CONCENTRATED FLOW Segment #1 Segment #2 Segment #3 Grass Woods Surface Description Segment #1 Segment #2 Segment #3 0.15 0.40 Unpaved Unpaved Manning's "n" Surface Description 3.35 3.12 130.4 ft 1490.0 ft 2- Year, 24- Hr. Rain Fall (In) Flow Length (ft) 52.0 ft 48.0 ft 1154.60 1143.20 Flow Length (ft) Elevation Up (ft) 1158.60 1157.30 1143.20 1037.90 Elevation Up (ft) Elevation Down (ft) 1157.30 1154.60 0.087 0.071 Elevation Down (ft) Watercourse Slope (ft/ft) 0.025 0.056 4.8 4.3 Land Slope (ft/ft) Average Velocity (ft/Sec) Time Of Concentration (Mins) 5.19 7.99 Time Of Concentration (Mins) 13.2 min. Total 0.46 5.79 Total Sheet Flow Tc (Minutes): Shallow Concentrated Tc (Mins): 6.2 min. cApw rking\east01\d3580559\ Duke Energy Sweetwater TOCAsm POST-DA2 Culvert DA Subcat Reach on Link Sweetwater HydroCAD Type 11 24-hr 10-yr, 24-hr Rainfall=5.34" Prepared by HDR, Inc Printed 12/15/2023 HydroCAD® 10.10-7b s/n 07102 © 2022 HydroCAD Software Solutions LLC Page 2 Time span=0.00-72.00 hrs, dt=0.02 hrs, 3601 points Runoff by SCS TR-20 method, UH=SCS, Weighted-CN Reach routing by Stor-Ind+Trans method - Pond routing by Stor-Ind method Subcatchment1S: Culvert DA Runoff Area=38.000 ac 0.00% Impervious Runoff Depth=2.21" Tc=19.4 min CN=69 Runoff=93.46 cfs 6.992 at Total Runoff Area = 38.000 ac Runoff Volume = 6.992 of Average Runoff Depth = 2.21" 100.00% Pervious = 38.000 ac 0.00% Impervious = 0.000 ac Sweetwater HydroCAD Type 11 24-hr 10-yr, 24-hr Rainfall=5.34" Prepared by HDR, Inc Printed 12/15/2023 HydroCADO 10.10-7b s/n 07102 © 2022 HydroCAD Software Solutions LLC Page 3 Summary for Subcatchment 1S: Culvert DA Runoff = 93.46 cfs @ 12.13 hrs, Volume= 6.992 af, Depth= 2.21" Runoff by SCS TR-20 method, UH=SCS, Weighted-CN, Time Span= 0.00-72.00 hrs, dt= 0.02 hrs Type II 24-hr 10-yr, 24-hr Rainfall=5.34" Area (ac) CN Description 38.000 69 Composite CN 38.000 100.00% Pervious Area Tc Length Slope Velocity Capacity Description (min) (feet) (ft/ft) (ft/sec) (cfs) 19.4 Direct Entry, Subcatchment 1S: Culvert DA Hydrograph 100 95 90 I 93.46cfs I I I I I I I I I I I I I I I I I I I I I I I I I I I I I _ _ 1 I _ I_ I_ I_ _ _I _I _I �1 1 1 1 1 1 1 1 1 IType lil 24-h �i ❑Runoff -_ 85 III_ _ _I _I _I I I I I I I I I I IIIIIIIIII I I I I���j I`, I 80 _ I_ I_I_ _I _ I_ I_ I_I_I_I _I _I _I — fir- 75 L 1- 1-1- 1 -1 J J J 1 1 1 1 L L L L L I- 1241hIr-RWnf61[6J 134` 70 65 1 1 1- - I- I- - -1-1--]A-444 -kt- I I I I 1 1/1���-t-44n�-k�� 1 1 -1 -4 -4 4 4 4- - i-RAinQf�%lAr�ma=p.78. 00- aac 55 P I I- -I -I -I fi fi fi fi 10 1;IOLIM T �"t``F'� 0 45 -1 1 1- -1-1-1-1-17TTTT777 IRuln6WQe-Oth�22V- il:- 1- I- 1- 1 1 -1 -1 -T 7 T T T T T 7 7 1- 1- 1-1-1 -1 -1 -1 .7 T T T T T 1 1 1 7 T T T T 1 1 1 1 1 1 1 1 T ,� 19.4 M1m 35 30 25 20 15 _II_ IIIII 10 0 2 4 6 8 10 12 14 16 18 20 22 24 26 28 30 32 34 36 38 40 42 44 46 48 50 52 54 56 58 60 62 64 66 68 70 72 Time (hours) Eastern Band of Cherokee Indians I Cherokee Trout Hatc Civil Calculations ��� Appendices Appendix E — Culvert Calculations HY-8 Culvert Analysis Report Crossing Discharge Data Discharge Selection Method: Specify Minimum, Design, and Maximum Flow Minimum Flow: 93.46 cfs Design Flow: 93.46 cfs Maximum Flow: 93.46 cfs Table 1- Summary of Culvert Flows at Crossing: Duke SW Headwater Total Culvert 1 Roadway Iterations Elevation (ft) Discharge Discharge Discharge (cfs) (cfs) (cfs) 1036.98 93.46 93.46 0.00 1 1036.98 93.46 93.46 0.00 1 1036.98 93.46 93.46 0.00 1 1036.98 93.46 93.46 0.00 1 1036.98 93.46 93.46 0.00 1 1036.98 93.46 93.46 0.00 1 1036.98 93.46 93.46 0.00 1 1036.98 93.46 93.46 0.00 1 1036.98 93.46 93.46 0.00 1 1036.98 93.46 93.46 0.00 1 1036.98 93.46 93.46 0.00 1 1040.50 202.72 202.72 0.00 Overtopping Rating Curve Plot for Crossing: Duke SW Total Rating Curve Crossing: Duke SW 1040.! 1040A 1039.! a 1039.1 w a5 m 1038.! m aD z 1038A 1037.! 1037A V V V TV Total Discharge (ds) V V V V « Culvert Data: Culvert 1 Table 1- Culvert Summary Table: Culvert 1 Total Culve Head Inle Outl Fl Nor Criti Out Tailw Outl Tailw Disch rt water t et ow mal cal let ater et ater arge Disch Elevat Cont Cont Ty Dep Dep De Dept Velo Veloc (cfs) arge ion rol rol pe th th pth h (ft) city ity (cfs) (ft) Dep Dep (ft) (ft) (ft) (ft/s (ft/s) th th ) (ft) (ft) 93.46 93.46 1036.9 3.24 3.50 7- 1.89 1.82 1.8 0.34 7.66 45.23 cfs CfS 8 0 M2 2 C 93.46 93.46 1036.9 3.24 3.50 7- 1.89 1.82 1.8 0.34 7.66 45.23 cfs CfS 8 0 M2 2 C 93.46 93.46 1036.9 3.24 3.50 7- 1.89 1.82 1.8 0.34 7.66 45.23 cfs CfS 8 0 M2 2 C 93.46 93.46 1036.9 3.24 3.50 7- 1.89 1.82 1.8 0.34 7.66 45.23 cfs CfS 8 0 M2 2 C 93.46 93.46 1036.9 3.24 3.50 7- 1.89 1.82 1.8 0.34 7.66 45.23 cfs cfs 8 0 M 2 2 c 93.46 93.46 1036.9 3.24 3.50 7- 1.89 1.82 1.8 0.34 7.66 45.23 cfs cfs 8 0 M 2 2 c 93.46 93.46 1036.9 3.24 3.50 7- 1.89 1.82 1.8 0.34 7.66 45.23 cfs cfs 8 0 M 2 2 c 93.46 93.46 1036.9 3.24 3.50 7- 1.89 1.82 1.8 0.34 7.66 45.23 cfs cfs 8 0 M 2 2 c 93.46 93.46 1036.9 3.24 3.50 7- 1.89 1.82 1.8 0.34 7.66 45.23 cfs cfs 8 0 M 2 2 c 93.46 93.46 1036.9 3.24 3.50 7- 1.89 1.82 1.8 0.34 7.66 45.23 cfs cfs 8 0 M 2 2 c 93.46 93.46 1036.9 3.24 3.50 7- 1.89 1.82 1.8 0.34 7.66 45.23 cfs cfs 8 0 M 2 2 c Culvert Barrel Data Culvert Barrel Type Straight Culvert Inlet Elevation (invert): 1033.48 ft, Outlet Elevation (invert): 1032.60 ft Culvert Length: 40.01 ft, Culvert Slope: 0.0220 Culvert Performance Curve Plot: Culvert 1 1040.� 1040.0 1039.� a } 1039.0 a) w 1038.0 co m a) z 1038.0 1037.� 1037.0 Performance Curve Culvert: Culvert 1 0 0 Inlet Control Elea Outlet Control Elev IUU IGU 14U IOU IOU GUU GGU Total Discharge (ds) Water Surface Profile Plot for Culvert: Culvert 1 Crossmg - Duke SW, Design Discharge - 93.5 cfs Cuh-ert - Cuh-ert 1. Culvert Discharge - 93.5 cfs 1040 1039 1038 1037 C 1036 } aD w 1035 1034 1033 1032 ACCESS ROAD 83" x 57" ELLIPTICAL CSP WATER PROFILE HGL 1' STREAM �EMBEDM�ENT -------x 10 -5 0 5 10 15 20 25 30 35 40 45 50 Station (ft) Site Data - Culvert 1 Site Data Option: Culvert Invert Data Inlet Station: 0.00 ft Inlet Elevation: 1032.48 ft Outlet Station: 40.00 ft Outlet Elevation: 1031.60 ft Number of Barrels: 1 Culvert Data Summary - Culvert 1 Barrel Shape: Elliptical Barrel Span: 83.00 in Barrel Rise: 53.00 in Barrel Material: Concrete Embedment: 12.00 in Barrel Manning's n: 0.0340 (top and sides) Manning's n: 0.0350 (bottom) Culvert Type: Straight Inlet Configuration: Thin Edge Projecting (Ke=0.9) Inlet Depression: None Tailwater Data for Crossing: Duke SW Table 2 - Downstream Channel Rating Curve (Crossing: Duke SW) Flow (cfs) Water Velocity Depth (ft) Shear (psf) Froude Surface (ft/s) Number Elev (ft) 93.46 1032.94 0.34 45.23 64.46 13.58 93.46 1032.94 0.34 45.23 64.46 13.58 93.46 1032.94 0.34 45.23 64.46 13.58 93.46 1032.94 0.34 45.23 64.46 13.58 93.46 1032.94 0.34 45.23 64.46 13.58 93.46 1032.94 0.34 45.23 64.46 13.58 93.46 1032.94 0.34 45.23 64.46 13.58 93.46 1032.94 0.34 45.23 64.46 13.58 93.46 1032.94 0.34 45.23 64.46 13.58 93.46 1032.94 0.34 45.23 64.46 13.58 93.46 1032.94 0.34 45.23 64.46 13.58 Tailwater Channel Data - Duke SW Tailwater Channel Option: Rectangular Channel Bottom Width: 6.00 ft Channel Slope: 3.0000 Channel Manning's n: 0.0260 Channel Invert Elevation: 1032.60 ft Roadway Data for Crossing: Duke SW Roadway Profile Shape: Constant Roadway Elevation Crest Length: 50.00 ft Crest Elevation: 1040.50 ft Roadway Surface: Gravel Roadway Top Width: 20.00 ft Eastern Band of Cherokee Indians I Cherokee Trout Hatc Civil Calculations ��� Appendices Appendix F — Riprap Calculations Appendices 20 10 0 Culvert diameter is 72" with 12" embed. Use Do=60" for riprap calculations 3a ��I Outlet w = Do + to pipe diameter (Do) La T flwater - 0.51)Q ot` � IZP t of p� 6ve 50 Discharge {ft3/sec} ,I 80 200 Q,o = 95 cfs Used: La = 32' 3Do = 18' W=22' 2 0 Ln a 1 a — d=60 .1..J 0 1000 Curves may not be extrapolated. Figure 8.06a Design of outlet protection protection from a round pipe flowing full, minimum tailwater condition (Tw r 05 diameter). Rev. 12/93 Use Class 2 Riprap: dso = 14" d_ = 28" depth = 2.5' 8.06.3 Trapezoidal Riprap-Lined Waterway Design.xlsm Landowner Duke Energy County Catawba County V 1.2015 Computed By VH Date 12/15/2023 1/15/2015 Checked by KM Date 12/18/2023 Note: Macros must be enabled in this spreadsheet in order for the "Solve" button to work. Design flow, Q= 93.46 cfs Slope, S= 0.05 ft/ft = 20.00 :1 Bottom Width, W= 6 ft Side slope, Z= 5 :1 Safety factor= 1.2 Typically 1.2 Rock shape = Angular Min. req'd D50= 8.10 in D50 used= 14.00 in n= 0.045 Freeboard= 0.25 ft WW horiz. Length= 32.0 ft U/S WW F.L. elev= 1036.0 ft D/S WW F.L. elev= 1034.4 ft Waterway drop= 1.6 ft WW length along slope= 32.0 ft Spreadsheet formatting key: XXX =Input cells X.XX =Output from "Solve" button X.XX =Other computed output Red text =Instructions, warnings, info Flow depth, d= 1.21 ft Calculated Critical depth, dc= 1.36 ft Critical slope, Sc= 0.031 ft/ft 0.7Sc = 0.0214 ft/ft 1.3SC = 0.0397 ft/ft Design slope, S= 0.0500 ft/ft Design slope OK. Flow is Supercritical. Velocity= 6.41 fps Est. riprap unit wt= Rock shape = Angular Rock Gs = Riprap thickness: Minimum= 2.33 ft Provided= 2.50 ft Sideslope height: Minimum= 1.46 ft Provided= 1.60 ft 1.4 Tons/CY 2.65 Required riprap gradation for D50 selected Rock dia., inches Rock weight, lb Smaller min. max. min. max. 100 21.0 28.0 675 1600 85 18.2 25.2 439 1166 50 14.0 21.0 200 675 10 1 11.21 18.2 1021 439 8.0 ft 6.0 ft 1.6 ft �-----------Riprap----- ''' \� Quantities: Riprap volume= 104.8 CY �� 6.5 ft Approx. weight= 146.7 Tons Geotextile WW CROSS SECTION Geotextile area= 303.7 SY* 32.0 ft *Geotextile area includes actual covered 2.5 ft 1 ----- surfaces only (no extra Riprap 20.00 ; for laps or anchorage) Geotextile WW PROFILE FYZ HDR Engineering, Inc. of the Carolinas 440 South Church Street, Suite 1200 Charlotte, NC 28202 NC License F-0116 hdrinc.com © 2023 HDR, Inc., all rights reserved