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PERMFILE71374
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PERMFILE71374
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Last modified
8/24/2016 11:20:40 PM
Creation date
11/20/2007 11:48:56 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1982057A
IBM Index Class Name
Permit File
Doc Date
3/13/2003
Section_Exhibit Name
Tab 21 Minesoil Reconstruction
Media Type
D
Archive
Yes
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The recommended topsoil salvage depth is based solely on the depth to sandstone hedrock. <br />The mean in situ suitable topsoil depth for 30 4inevada profiles is 28 inches (Appendix <br />9-6). <br />The 53C, 53D, 53E, end 53F map units consist of 85 percent Vinevede with 5 percent <br />Splitro, 4 percent Coutis, 4 percent Foidel, 1 percent Roxal variant, end 1 percent <br />Starman inclusions (Appendix 9-2, Table 1). A 2.0-foot mean salvage depth was used for <br />Nap Units 53C, 53D, 53E, and 53F to calculate recoverable topsoil volumes listed in Table <br />21-1 and Exhibit 9-7. This topsoil salvage depth figure accounts for inclusions and <br />topsoil loss during salvage due to brush clearing. <br />62C, 62D-Chaperton Sandy Clay Loam. The Chaperton sandy clay loam soil occurs on strongly <br />sloping to moderately steep mountain toeslopes, sideslopes, end alluvial fens. This soil <br />has more profile development (structurally developed subsurface horizon) then the adjacent <br />Torriorthents but lacks the thick, dark colored surface horizon associated with Silas. <br />This soil is a good source of loamy topsoil. The mean in situ suitable topsoil depth for <br />• 3 Chaperton profiles is 60 inches (Appendix 9-b). <br />The 62C and 62D map units consist of 85 percent Chaperton with 8 percent Torriorthents end <br />7 percent Silas inclusions (Appendix 9-2, Table 1). A 4.5-foot mean salvage depth was <br />used for these map units to calculate recoverable topsoil volumes listed in Table 21-1 end <br />Exhibit 9.7. This topsoil salvage depth figure accounts for inclusions within these map <br />units. - <br />66D-Foidel Silt Loam. The foidel silt loam soil is located on moderately steep mountain <br />sideslopes, ridgeline benches, and sweles. The soil profile is deep and well developed <br />with a thick, dark colored surface horizon and subsoil clay accumulation. Adjacent soils <br />have higher subsoil clay contents (ROUtt and Coche[opa) or lack subsoil clay accumulation <br />(Coutis end Vinevada). <br />The recommended topsoil salvage depth is typically based on the entire soil profile since <br />all horizons have favorable chemical and physical properties. Occasionally, topsoil <br />salvage must be discontinued et the top of subsoil or substratum horizons which have <br />• unsuitable clay contents or consistency characteristics. The mean in situ suitable <br />topsoil depth for 19 profiles is 57 inches (Appendix 9-6). <br />79 Revised 04/24/97 <br />
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