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SL -9 <br />The Universal Soil Loss Equation will be used to calculate the soil loss from the reclaimed areas, <br />and the shadscale reference area to determine if untreated drainage from the reclaimed mine site <br />is contributing suspended solids in excess of premining levels. The following <br />sediment volume calculation is prepared in accordance with U. S. Department of Agriculture, Technical <br />Notes, Agronomy Note #50, dated January, 1977. The maps and figures utilized in the LISLE calculations <br />are obtained from the referenced Agronomy Note #50. <br />The reclaimed areas are broken into seven separate areas for evaluation; Ponds 7, 9, Ponds 6 & 10, <br />Pond 13 and associated permanent drainages, CBA Sump #1 CRDA Road and the G Substation, . <br />USING THE UNIVERSAL SOIL LOSS EQUATION <br />R (rainfall) factors are assigned by geographical regions based on weather data furnished by the U.S. <br />Weather Service R values are based on rainfall amount, time, and intensity In the mountains, R values <br />were computed primarily for valley areas and have been increased to account for run-off from snow melt. <br />The R factor of 30 used for this calculation is derived from an iso-erodent map, presented in the referenced <br />Agronomy Note #50, and is the same for both the reclaimed slopes and the adjacent natural slope. <br />K (soil erodibility) factors are assigned to each soil series and they are used to predict the erodibility of a <br />soil and its tolerance to erosion in relation to specific kinds of land use and treatment Soils having the <br />highest K value are the most erodible. The K value used for this calculation is derived from data from the <br />U.S Department of Agriculture Soil Survey, Web Soil Survey, and is based on the soils classification <br />of 15 -Cameo Fine Sandy Loam. SedCad was used to select the X' Factor. <br />The K factor for the soil is 0.24 <br />LS (length and percent slope) factors account for the length and percent slope. These factors are taken <br />from Figure 4 of this document. Length of slope begins at the top of the micro watershed This is usually at <br />the top of a hill, ridge, terrace or diversion. The length of slope is considered to end for a given field at one <br />of the following places: (1) the point where the slope decreases to the extent that deposition occurs, (2) <br />the point where runoff enters a well-defined channel, terrace or diversion , or (3) where water leaves the field <br />The LS for the Reclaimed Areas are defined by the length and slope gradient within the distrubed area <br />LS factors for the adjacent areas are drawn immediately adjacent to the disturbed area boundary for <br />the reclaimed areas. <br />Adjacent Area (CBA #2) - LS Factor <br />The LS factor for the Adjacent area is based on an average 35H:1 V Slope and an average <br />change in elevation of 4 feet and average length of slope is 139 feet based on two flow lines located in the <br />adjacent area. <br />Average Length 1390 Feet <br />Average Slope 30% <br />Percent Slope (S) <br />20% 3.0% 4.0% <br />120 0 210 0.300 0 430 <br />139.0 "LS" Factor 0.319 <br />140 0 220 0 320 0 460 <br />CBA #2- LS Factor <br />The LS factor for CBA #2 Area is based on an average 33H.1 V slope at an average <br />change in elevation of 4 feet based on two flow lines cut through the reclaimed area. <br />Average Length 130.0 Feet <br />Average Slope 30% <br />Percent Slope (S) <br />2.0% 3.0% 4.0% <br />120 0 210 0.300 0 430 <br />130.0 "LS" Factor 0.310 <br />140 0.220 0.320 0.460 <br />Tab -9, Page 6 <br />Revised 10/18/2016 <br />