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• TABLAcontinued) • <br />RD&D LEASE COC-69166 <br />SOIL TINTEMEIA IMINS <br />8 <br />Typical Reaction Class: narrative range of pH of surface (A horizon)/subsoil (B horizon, or if B is lacking, the first C horizon). <br />Reaction Description pH Range <br />Strongly Acid 5.1-5.5 <br />Medium Acid 5.6-6.0 <br />Slightly Acid 6.1-6.5 <br />Neutral 6.6-7.3 <br />Mildly Alkaline 7.4-7.8 <br />Moderately Alkaline 7.9-8.4 <br />Strongly Alkaline 8.5-9.0 <br />Very Strongly Alkaline <9.0 <br />Soils that are mildly alkaline usually are calcareous. Soils of moderate alkalinity or stronger are assumed to be calcareous. Strongly alkaline soils have increased sodium concentrations. <br />9 <br />Wind Erodibility Group (WEG): This is an arbitrary grouping of soils based on texture and aggregation. Values range from 1 to 8, with lower numbers indicating increased susceptibility <br /> to wind <br />erosion. The Wind Erodibility Group classification is for the surface layer only, but could be applied to any layer within a soil profile. Class are defined in the National Soils Handbook <br /> (USDA-NRCS <br />2007). <br />WEG Soil Texture of Surface Laver <br />Very High Erodibility 1 Very fine sand, fine sand, sand, or coarse sand (I = 220)* <br />2 Loamy very fine sand, loamy fine sand, loamy coarse sand (I = 134) <br />High Erodibility 3 Very fine sandy loam, fine sandy loam, sandy loam, or coarse sandy loam (I = 86) <br />4 Clay, silty clay, noncalcareous clay loam, or silty clay loam with more than 35 percent clay content (I = 86) <br />4L Calcareous loam and silt loam, or calcareous clay loam, and silty clay loam (I = 56) <br />Medium Erodibility 5 Noncalcareous loam and silt loam with less than 20 percent clay content, sandy clay loam, or sandy clay (I = 56) <br />6 Noncalcareous loam and silt loam with more than 20 percent clay content, or noncalc.clay loam with less than 35 percent clay content (I = 48) <br />Low Erodibility 7 Silt, noncalcareous silty clay loam with less than 35 percent clay content (I = 38) <br />8 Soils not suitable for cultivation due to coarse fragments or wetness, wind erosion not a problem (I = ) <br />HEL (Wind) and HEL (Water) status taken from "Highly Erodible Soil Map Unit List (HEL), dated 1/1/90 (NRCS 2001). <br />* I Factor: This value indicates the relative amount of soil that can be expected to erode, through wind influence, in Tons-Per-Acre-Per-Year (T/AC/YR). It is related to the wind erodibility <br /> group <br />number and the percent of dry soil aggregates >0.84 mm in diameter. <br />10 <br />Water Erosion Hazard: taken from Soil Survey of Rio Blanco County (Tripp et. al. revised 1992). HEL Water list (NRCS 2001). Water erosion hazard rating includes many factors including <br /> the <br />surface soil, precipitation, length, and steepness of slope. <br />u <br />K Factor: This value indicates the relative susceptibility of a surface soil to water erosion. Values may range from 0.00 to 0.70. Higher K values indicate higher erosion susceptibility. <br /> Soils with K <br />factor over about 0.40 are generally considered to be highly susceptible to water erosion. It should be noted that the K factor is derived primarily from physical characteristics of <br /> the soil, and does not <br />reflect other soil erosion factors such as management practices, precipitation, or length and steepness of slope. <br />Erodibility Potential "K" Value <br />Low Erodibility 0.20 or less <br />Moderate Erodibility 0.21 to 0.40 <br />High Erodibility >0.40 <br />20