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PERMFILE54536
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Last modified
8/24/2016 10:57:36 PM
Creation date
11/20/2007 4:12:23 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Section_Exhibit Name
EXHIBIT 27 CHARACTERISTICS OF WEST ELK MINE SOIL MAPPING UNITS
Media Type
D
Archive
No
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<br />Mountain Coal Company Exhibit 27 <br />West Elk Mine Characteristics of West Elk Mine Soil Mapping Units <br />The soils of this unit are medium to moderately fine textured and are subject to packing <br />if traversed by heavy machines, or to irreversible puddling if they are handled wet. The} <br />can be worked over a moderate range of soil moisture, but any work involving relocation <br />of the soils will require good management to insure continued good physical conditions. <br />These soils are considered good sources of seedbed materials. <br />The soils of this unit have moderate shrink/swell ratios. Total potential extensibility for <br />a 40-inch section ranses from 0.8 to 2.0 inches. <br />In their natural state. [hese soils are not subject to accelerated erosion by either wind or <br />water unless natural vegetation has been destroyed or depleted. If cleared and disturbed. <br />they are moderately susceptible to mass movement especially when very wet. <br /> <br />Chemical ProQerties and Natural Fertility - These soils are moderately weathered, <br />maturely developed units having genetic soil horizons of silicate clay accumulation (B2t <br />horizons) but normally lacking horizons of secondary carbonate accumulation. The soil <br />solum (A and B horizons) is neutral to mildly alkaline in reaction while the C horizon <br />is neutral to moderately alkaline and may contain some free carbonate. Under such <br />conditions, the cation exchange complex (portion of the soil having an ability to hold and <br />exchange cations) is base saturated with the calcium cation, but there is not enough free <br />calcium and magnesium carbonate to seriously depress the availability of other plant <br />nutrients. Natural fertility levels are high in the upper horizons of the soil, gradually <br />decreasing with depth as organic content decreases. Nitrogen supplies and availability <br />are closely related with the amount and decomposition of soil organic matter. Any <br />practice that alters the amount of soil organic matter or causes more rapid decomposition <br />of organic matter will directly affect nitrogen levels in the soil. <br />No evidence of deficiencies of essential plant nutrients or trace elements is noted. but <br />evidence of borderline phosphorus deficiency is indicated by the soil analysis (see <br />Exhibit 26). Temporary fertilization programs for disturbed areas that are being <br />revegetated should include supplemental additions of nitrogen and phosphorus to insure <br />the best possible seedling growth and vigor. <br />Mappine Unit Number X30 -This mapping unit has the same description as mapping <br />unit number 30. <br /> <br />Exhibit 2 i-23 <br />
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