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:\'urrnrhrr 199% CYCC'-.ti~•dinr~nr ))cld Drnnm.arurirnr-rblirrc• 3 .-1 <br />Hydru~raph Response Shape. A unit hydrograph was chosen for each drainage area or sub-area model to <br />• predict thr runoff response. The hydrograph responses available in the SEDCAD+ model are slow, medium, <br />and fast. A slow response corresponds to a forested area or an area with a number of obstructions, where as a <br />Last rcsponsc corresponds to an unve,~etated or poorly protected area. For the demonstration, a medium runoff <br />response was chosen. <br />Drainage Basin Area. Representative one acre drainage basin areas were modeled for [he reclamation block <br />and reference area being evaluated. Represen[auve one acre unmined drainage areas were modeled to exhibit <br />overland (low throughout die length of [he defined watershed. Representative one acre mined drainage areas <br />were divided into tour sub-watersheds due to the presence of contour fwrows throughout the reclamation <br />blocks. Within these areas, overland Flow lengths are shortened with subsequent Flow paths consisting of <br />overland drainage, contour furrow Clow, and then combined Flow along grassed waterways representative of <br />areas of concentrated runoff. <br />Time of Concentration. Time of concentration (tc) within each representative one acre drainage was <br />calculated with SEDCAD+ using [he SCS Upland Method, as presented in Barfield, e[ al. (1981), page 100. <br />Representative one acre areas were used to derive hydraulic lengths and drainage paths. Average slopes for <br />Blocks North and South were measured directly from I" = 500' scale maps. These slopes were used as inputs <br />for calculating both time of concentration and Muskingum routing parameters where appropriate. Slopes of the <br />contour furrows in the reclaimed blocks were assumed at 0.5 %. <br />Curve Number. The runoff curve number (CN) is a factor relating the amount of rainfall to the amount of <br />runoff for a given area. It is dependent upon the infiltration characteristics of site-specific soil types and the <br />type and amount of vegetation. Prior to disturbance, the mined areas encompassed the following soil types <br />• (Ref: Soils Map, CYCC Permit No. C-84-062): <br />SOIL NAME HYDROLOGIC SOIL GROUP <br />Buckskin Loam C <br />Routt Loam C <br />Binco Silty Clay Loam D <br />Unnamed Loam - <br />Aaberg Silty Loam D <br />Splitro Sandy Loam C <br />Parachute -Merino Complex C <br />Hydrologic Soil Groups based on Routt County SCS designations. '~ <br />Soil groups for the reclaimed blocks are assumed to be a mixture of the groups which were originally stripped. <br />Ground cover values for the Mine 3 North, Mine 3 South, Dryland Reference, Low Sage Reference, and the <br />Pastureland Reference Areas were obtained from the 1995, 1996, and 1997 vegetation surveys conducted by <br />CYCC. Curve numbers were obtained from the SEDCAD+ selection tables based on soil type and vegetative <br />condition. Curve numbers were determined for the following conditions: <br />Block North <br />Hydrologic Soil Group: Predominantly D <br />Land Use Description: Pasture/Range <br />Condition: Good <br />• Cover Type: Grass <br />CN: 80 <br />r\bon d rc I \m i ne3\scdkcdm inc J.doc <br />