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NUCLA PR NO. 2 <br /> natural in-place densities can range in the area of 90-110 pounds per <br /> cubic feet. Sediment in a pond can range from 80-100 pounds per cubic <br /> feet depending on water content, organic content, coal content and <br /> particle distribution of the sediment, etc. Based on Lara and Pemberton <br /> (Design of Small Dams) equation the following calculations can be <br /> performed. <br /> Assumptions: <br /> Sandy Loam (Tab 9) : <br /> % clay = 5% = pc <br /> % silt = 25% = pm <br /> % sand = 70% = ps <br /> Operation Type (1) = Sediment always submerged or near submerged. <br /> eq. W = We (pc) + Wm (pm) + Ws (ps) <br /> 3 <br /> We = 26 lb/ft <br /> 3 <br /> Wm = 70 lb/ft <br /> 3 <br /> Ws = 97 lb/ft <br /> W = 26 (0.05) + 70(0.25) + 97(0.70) <br /> 3 <br /> W = 1.3 + 17.5 + 67.9 + = 86.7 lb/ft <br /> Miller (Design of Small Dams) developed an equation for determining the <br /> average density of all sediment deposited in T years of operations of a <br /> reservoir as follows: <br /> T <br /> WT = W1 + 0.4343 K T-1 (loge T) - 1 <br /> where: <br /> 3 <br /> W1 = 86.7 lb/ft <br /> K = Ks(ps) + Km(pm) + Kc(pc) <br /> K = 0(0.70) + 5.7(0.25) + 16.0(0.05) <br /> K = 0 + 1.4 + 0.8 = 2.2 <br /> T = 2 years <br /> 2 <br /> W2 = 86.7 + 0.4343(2.2) [2-1 (loge 2) - 1] <br /> 3 <br /> W2 = 86.7 + 0.96 [0.386] = 87.1 lb/ft <br /> 3 <br /> Use 87 lb/ft <br /> 20 <br />