Laserfiche WebLink
<br />I <br />I <br />I <br />I <br />,- <br />, <br />I <br />I <br />- <br />il <br />II <br />I~ <br />I <br />:~ <br />I <br />I <br />G <br /> <br />" <br />:! <br />I <br />. <br /> <br />I <br /> <br />basin. This procedure assigns a curve number to each of four <br />soil groupings and then modifications are made to account for <br />the other variables. The four hydrologic soil groups, according <br />to their infiltration and transmission rates, are: <br /> <br />GROUP A Low runoff potential. Soils having high infiltration <br />rates even when thoroughly wetted. These consist chiefly <br />of deep, well to excessively drained sands or gravel. <br />These soils have a high rate of water transmission in <br />that water readily passes through them. <br /> <br />GROUP B Soils having moderate infiltration rates when thoroughly <br />wetted. These consist chiefly of moderately fine to <br />moderately course textures. These soils have a moderate <br />rate of water transmission. <br /> <br />GROUP C Soils having slow infiltration rates when thoroughly <br />wetted. These consist chiefly of soils with a layer <br />that impedes downward movement of water or soils with <br />moderately fine to fine texture. These soils have a <br />slow rate of water transmission. <br /> <br />GROUP D High runoff potential. Soils having very slow infiltra- <br />tion rates when thoroughly wetted. These consist chiefly <br />of clay soils with a high swelling potential, soils with <br />a permanent high water table, soils with a claypanor <br />clay layer at or near the surface, and shallow soils <br />over nearly impervious material. These soils have a <br />very slow rate of water transmission. <br /> <br />Appendix A lists the hydrologic soil types for El Paso and <br />Teller Counties. Maps and other information showing soil series <br />are available for viewing at local SCS offices. <br /> <br />For design purposes, the normal antecedent moisture condition <br />(AMC II) shall be used. Wet and/or dry antecedent moisture <br />conditions (AMC III and AMC I respectively) should only be used <br />for purposes of reproducing historical events. The curve numbers <br />given in this manual are for AMC II only. Figure 111-7 and 111-8 <br />show curve numbers corresponding to various conditions of cover <br />for range and urban soil cover complexes. Similar information <br />is presented in a tabular form in Tables 111-4 and 111-5. A <br />weighted CN for a given basin can be determined in a similar <br />manner as the composite C in the rational method. <br /> <br />n <br />~CN'A' <br />L...-J J. J. <br />i=l <br /> <br />CN = <br /> <br />At <br /> <br />where: <br /> <br />23 <br />