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r~ <br />L <br />Due to similarity in channel slopes and unit discharges, a single <br />riprap gradation can be utilized to stabilize the channels in every area <br />considered. Gradation criteria for the riprap are as follows: <br />Percent Finer Rock Diameter <br />By Weight (inches) <br />100 27 <br />50 18 <br />20 9 <br />10 6 <br /> <br />• <br />Tables 2 through 8 summarize the important hyoraulic, geometric and <br />riprap criteria applicable to the channels considered. Hydraulic <br />information is also found on Sheets 3 through 7. <br />Granular Bedding <br />Due to the relatively steep slopes and fine-grained nature of the <br />underlying material, a granular filter layer is required beneath the <br />riprap. Generalized criteria for bedding specified in the Urban Storm <br />Drainage Criteria Manual specify either a two layer filter consisting of <br />Type I and Type II bedding meeting specifications given in Table 9, or <br />alternatively a one-foot thick layer of Type II bedding. <br />Estimated Quantities <br />Table 10 provides estimates of the quantities of riprap and granular <br />bedding required to construct the proposed channel improvements. <br />SEDIMENT YIELD CALCULATIONS <br />Soil loss in tons/acre/year and sediment yield in tons/year were <br />estimated for the major drainage channels of the Eckman Park Mine using <br />the Universal Soil Loss Equation (LISLE). Estimates were made for <br />approved and existing drainage ways (Table 11). Soil loss is converted <br />to sediment yield by multiplying by drainage area and by a sediment <br />delivery ratio. The latter is a percentage of the soil eroded which is <br />actually removed from the watershed rather than stored by depositional <br />processes. Sediment delivery ratio was determined using a relationship <br />between drainage area and sediment delivery ratio presented by <br />Wischmeier and Smith (1978). <br />The LISLE predicts soil loss (here expressed in tons/acre/year) on <br />the basis of five factors as follows: 1) rainfall and runoff factor <br />(R); 2) soil erodibility factor (K); 3) topographic factor (LS, <br />incorporating slope-length (L) and slope gradient (S)); 4) cover and <br />