My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
PERMFILE71374
DRMS
>
Back File Migration
>
Permit File
>
800000
>
PERMFILE71374
Metadata
Thumbnails
Annotations
Entry Properties
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
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
43
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
Lymanson variant has a shallow profile whereas Teton profiles are moderately deep. • <br />Adjacent soils are shallow and lack subsoil clay accumulation (Splitro), have a thicker <br />mollic epipedon (Yinevada ), or have a light colored surface horizon (Aaberg). <br />The recommended topsoil salvage depth for both soils is based solely on the thickness of <br />the mollic epipedon and the depth to the unsuitable silty clay substratum. The in situ <br />suitable topsoil depth for 1 Lymanson variant profile is 13 inches (Appendix 9-6). The in <br />situ suitable topsoil depth for 1 Teton profile is 13 inches (Appendix 9-b). <br />The 33D map unit consists of 45 percent Lymanson variant and 45 percent Teton with 4 <br />percent Splitro, 3 percent Vincvada, and 3 percent Aaberg inclusions (Appendix 9-2, Table <br />1). A 1.0-foot mean salvage depth was used for this map unit to calculate recoverable <br />topsoil volumes listed in Table 21-1 and Exhibit 9-1. This topsoil salvage depth figure <br />accounts for inclusions and topsoil loss during salvage due to brush clearing. <br />34C, 34D - Coutis Silt Loam. Coutis silt loam soils occur on the strongly sloping to <br />moderately steep bedrock controlled concave sideslopes and upland swales or drainages. <br />The soil profile has a very thick, dark Color ed surface horizon which directly overlies a <br />thin C horizon and sandstone bedrock at 40 to 60 inches. Adjacent soils are shallower • <br />(Vinevada and Skyway), have a light colored surface horizon (Roxal variant end Starman), <br />or have more profile development with subsoil clay accumulation (Lymanson and Fo idel). <br />The recommended topsoil salvage depth is based primarily on the thickness of the mollic <br />epipedon end depth to sandstone bedrock. Topsoil salvage will typically be terminated at <br />the sandstone bedrock contact; however, salvage will be discontinued at a shallower depth <br />if loamy sand or skeletal strata is encountered above the bedrock. The mean in situ <br />suitable topsoil depth for 27 Coutis profiles is 51 inches (Appendix 9-6). <br />The 34C and 34D map units consist of 85 percent Coutis with 5 percent Foidel, 3 percent <br />Winevada, 2 percent each of Skyway, Roxal variant, and Lymanson, and 1 percent St arman <br />inclusions (Appendix 9-2, Table 1). <br />A 4.0-foot mean salvage depth was used for Xap Units 34C and 34D to calculate recoverable <br />topsoil volumes listed in Table 21-1 and Exhibit 9-1. This topsoil salvage depth figure <br />accounts for inclusions and topsoil loss during salvage due to brush clearing. <br /> • <br />16 Revised OG/24/91 <br />
The URL can be used to link to this page
Your browser does not support the video tag.