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PARTICLE SIZE DISTRIBUTION <br />The particle size distribution for the soils in the Johnson and Pyeatt drain- <br />ages was determined by averaging the results from 23 soil samples taken in [he <br />Johnson drainage basin. The results, along with the average composition of <br />the soil, are shown on Table E-1, Soil Composition in Johnson Drainage. Once <br />a percentage of sand, silt, and clay was determined, each class was broken <br />into five sub-sizes to give a particle size distribution with 15 values. The <br />particle size distribution 13 given in Table E-2, Particle Size Distribution. <br />SOIL ERODIBILITY FACTORS <br /> The soil erodibility factor, K, was determined using the soil compositions for <br /> disturbed and undisturbed land along with structure and permeabilCy factors. <br /> The soil erodibility factors for both disturbed and undis turbed land are shown <br /> on Tab 1e E-3, Soil Erodibility Factors. <br /> CONTROL-PRACTICE FACTORS <br />/ The control ~C) and practice ~P)~factors for use in th e ModiFied Universal <br />• Soil Loss Equation are shown in Table E-G, Sedimentology Parameters. <br /> <br /> REVISED FFR 1 ~ '87 <br />