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<br />' SOILS REPORT <br />SNOWMASS COAL COMPANY <br />SEPTEMBER 23, 1987 <br />' Twelve samples of soil taken from the Snowmass Coal Company's re vegetation <br />were presented for analysis in September, 1987. The soils were air-dried and <br />' ground to pass through a 1 mm sieve. A portion was withheld from the grinding process <br />for textural analysis. Some fragments of shale were present in several of the samples <br />' and these fragments were removed from the samples for the textural analysis. The <br />' remainder of each sample was subjected to accepted chemical and physical analyses. <br />FERTILITY RESULTS <br />' The fertility of the soils is quite typical of most western Colorado soils <br />developed over or near marine shale formation. Where precipitation is adequate, <br />' the soils will support varied and relatively abundant plant growth. However, nitrogen <br />~~5,~~a <br />' and phosphorus levels are generally low. Potassium and copper levels are adequate <br />and iron, zinc and manganese levels are abundant. Table 1 shows the sample descriptions <br />as written on the sample containers. The sample designated by "I", or the #1 mine <br />fan site soil, is by far the most fertile. See table 2 for individual soil fertility <br />' results. The coal/soil sample, "X", is the least fertile. Fertilizer recommendations <br /> will be found at the conclusion of this report. <br />' <br /> SALINITY RESULTS <br /> <br />' The saliniti es of the soil sample are in the medium to low ranges and reflect <br /> a good drainage i n the soils. The pH's of the soils are acceptable and are quite <br />t common to the pH' s of the soils of the area. Only one of the samples ( "I") had <br /> an acid pH. The sodium adsorpt ion ratios indicate a low sodium hazard and infiltration <br />1 it <br />f <br />i <br />ti l <br />h <br />b i <br />i <br /> prec <br />o <br />p <br />a <br />on ou <br />d not <br />s <br />e h <br />ndered by excess sod <br />um. See table 3 for specific <br />' results. <br /> <br />