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2017-02-03_PERMIT FILE - C1980004 (25)
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2017-02-03_PERMIT FILE - C1980004 (25)
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Last modified
7/13/2017 8:56:29 AM
Creation date
7/13/2017 8:46:16 AM
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Template:
DRMS Permit Index
Permit No
C1980004
IBM Index Class Name
Permit File
Doc Date
2/3/2017
Section_Exhibit Name
Appendix T Proposed Expansion Area
Media Type
D
Archive
No
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strongly effervescent; from lab data: pH=8.7 (strongly alkaline), EC=3.95 (very slightly <br />saline), SAR=26.9 (highly sodic); OM=1.9% (medium); gradual wavy boundary. <br />C4 horizon — 60 to 96 inches (5 to 8'); light yellowish brown (10YR 6/4) sandy loam with <br />about 5% mixed gravels,yellowish brown (10YR 5/4) moist; massive structure; very hard <br />dry consistence, firm moist consistence, and slightly sticky and slightly plastic wet <br />consistence; strongly effervescent; from lab data: pH=8.2 (moderately alkaline), EC=6.21 <br />(slightly saline), SAR=28.1 (highly sodic); OM=1.4% (medium); gradual wary boundary; did <br />not hit bedrock. <br />Unnamed fine sandy loam (Map Unit 1) Topsoil Suitability and Recommended <br />Salvage Depth: Topsoil 10"/ Subsoil 10" <br />The topsoil suitability and recommended salvage depth of Map Unit I is the same as Map <br />Unit H. The upper 20 inches of Unnamed fine sandy loam (Map Unit 1) is entirely "suitable" <br />(WDEQ, 1996) and could be salvaged for use in subsequent future reclamation. This <br />topsoil and upper subsoil material is both nonsaline and nonsodic and has good soil texture <br />and organic matter content. Below about 20 inches in depth, Unnamed fine sandy loam <br />can have high exchangeable sodium (high SAR), low organic matter content, and coarser <br />textures in some profiles and this lower material is not recommended for salvage. The <br />upper 10 inches of Unnamed fine sandy loam is recommended for salvage as Topsoil and <br />the underlying 10 inches recommended for salvage as Subsoil. <br />3.3 Map Unit G: Rock Outcrop — Loamy -skeletal Torriorthents complex, 15 to 90% <br />slopes <br />Rock Outcrop — Loamy -skeletal Torriorthents (Map Unit G) is mapped on the moderately <br />sloping to very steep bedrock cliffs and lower slopes located on the east side of the study <br />area. The bedrock is sedimentary strata of the Cretaceous Mesa Verde Formation which <br />includes the dominant interbedded sandstone and shale strata but also carbonaceous <br />shale and at least one thin coal seam. The map unit is composed of about 75 percent <br />Rock Outcrop and very shallow soils less than 4 inches to bedrock, and about 25 percent <br />undifferentiated Torriorthents (shallow to deep, fine -loamy to loamy-skeletal).Torriorthents <br />are located on the lower slopes in short alluvial fan or talus slope positions, and Rock <br />Outcrop typically on the higher, very steep terrain. The two components are interspersed <br />in a sufficient complex pattern that does not allow separation at the mapping scale utilized <br />for the project. <br />Loamy -skeletal Torriorthents were fully described and sampled at one representative site, <br />M26, located in a delineation of Map Unit G. Rock Outcrop includes raw exposures of the <br />dominant sandstone and shale, talus areas with large rocks, and small areas with very <br />shallow soils less than 4 inches to bedrock. <br />-12- <br />
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