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2. Provide an emergency spillway capable of passing runoff from <br /> the 25-year, 24-hour storm event (0.33 ac-ft.). <br /> 3. Provide adequate storage for the sediment generated from the <br /> 10-year, 24-hour (MUSLE) storm event (2.9, 10-year, 24-hour <br /> MUSLE storm events or 0.07 ac-ft. ). <br /> 4. Provide a nonclogging dewatering device and principal spillway <br /> that will provide adequate detention time for the 10-year, <br /> 24-hour storm event and still allow a method to dewater the <br /> pond to the 100 percent sediment storage level in a reasonable <br /> amount of time. <br /> HYDROLOGY <br /> The hydrology of the watershed was analyzed by utilizing the SEDIMOT II <br /> computer modeling program. In performing this analysis, the <br /> characteristics of the minesite and reclamation procedures along with <br /> onsite sediment control procedures were considered. Addendums A, B, and <br /> C contain complete listings of the SEDIMOT II inputs and outputs for the <br /> 10-year, 25-year, and 100-year design storms, respectively. Table 1 is <br /> a summary of these results. <br /> TABLE 1 <br /> As-Built Hydrology and Sedimentology Summary <br /> Structure 002 <br /> DESCRIPTION 10yr-24hr 25yr-24hr 100yr-24hr <br /> Precipitation Depth 1.60-in. 1.80-in. 2.40-in. <br /> Inflow Runoff Volume 0.257-ac-ft 0.334-ac-ft 0.593-ac-ft <br /> Pond Volume at Peak Stage 0.276-ac-ft 0.44-ac-ft 0.525-ac-ft <br /> Peak Stage 5.2 -ft 6.55-ft 7.15-ft <br /> Peak Inflow Rate 3.45-cfs 4.45-cfs 7.71-cfs <br /> Peak Discharge Rate 0.010-cfs 1.65-cfs 3.19-cfs <br /> Basin Trap Efficiency 99.1% --- --- <br /> Detention of Flow (Sediment) 37.87-hrs --- <br /> Detention of Hydrograph Centers 16.52-hrs --- --- <br /> Input consists of precipitation amount (inches) , watershed area (acres) , <br /> time of concentration (hours) , runoff curve number (CN) , representative <br /> particle-size distributions of soils in the area, sedimentology <br /> information, spillway information, etc. The drainage area for Sediment <br /> Pond 002 was determined from a 1" = 400' topographic map (see Exhibit <br /> 13-4) . <br /> 2 <br />