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4-27 <br />Laboratory analyses of the sampled soils was conducted by F b L <br />• Labs, formerly in Fort Collins, Colorado, and by Colorado Analyt- <br />ical Consultants in Brighton, Colorado. The results from the <br />analysis of all of the samples are compiled by series on one <br />table; the original laboratory methods and results are included <br />as part of Appendix Es. <br />The mapping, pedon descriptions and chemical analyses were <br />compiled and interpreted for this report. Soils were classi- <br />fied to the series level and potential soil use information <br />was obtained from the SCS. The soils in the addendum area were <br />evaluated as a source material for reclamation, based on field <br />data, soil information acquired during the field visits, from <br />other soils assessments (WRD 1980a; 1980b; 1981), chemical and <br />physical analyses, and SCS data. <br />4.4.2 Soil Series Descriptions <br />The important characteristics of each major soil are listed in <br />• Table 4.4-1S. Characteristics include soil depth, drainage <br />class, slopes, parent material, and landform. The color, tex- <br />ture, and thickness of the surface, subsoil, and substratum <br />of a typical profile are described. The dominant native vege- <br />tation species, permeability, available water-holding capacity, <br />and effective rooting depth for the pedon are also included. <br />The table contains all the information usually reported in SCS <br />detailed series descriptions. All detailed pedon descriptions <br />of representative profiles are presented as part of Appendix Es. <br />Soils within the addendum area range from shallow to very deep, <br />with clayey to sandy textures. Shallow soils overlie bedrock <br />at depths less than 20 inches. They occur on gentle to extremely <br />steep slopes. These soils range in texture from silty clay looms <br />to very gravelly looms. The deeper soils are formed in alluvium, <br />colluvium, residuum, or eolian deposits and occur on nearly <br />level to moderately sloping flood plains and terraces, and nearly <br />• <br />