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2010-12-17_REVISION - C1981019 (142)
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2010-12-17_REVISION - C1981019 (142)
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Last modified
8/24/2016 4:28:03 PM
Creation date
1/29/2009 3:18:26 PM
Metadata
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Template:
DRMS Permit Index
Permit No
C1981019
IBM Index Class Name
REVISION
Doc Date
12/17/2010
Doc Name
Exhibit 9 Item 8 Baseline Survey of Soil Resources Collom Mining Area
Type & Sequence
PR3
Email Name
JRS
Media Type
D
Archive
No
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Baseline Survey of Soil Resources - Collom Mining Area July, 2006 <br />I <br />suitability thresholds for both boron and selenium in topsoil (WDEQ, 2004). All soils sampled fall below <br />the recommended limit of S.0 ppm for boron while one sample (0825-R01, 14-30 inches, Campspass <br />- 0.12ppm) minimally exceeded the marginal threshold of 0.1 ppm selenium. These results do not <br />support the need for further analysis, as it appears boron and selenium are found in low concentrations in <br />the parent materials of the Survey Area. <br />Soil Map Unit Descriptions <br />The soil survey identified 62 separate map units comprised of series, families, and other more generally <br />classified soils with broader ranges of characteristics. These map units are presented in Appendix B, <br />Table B-5. The map showing the distribution of the map units is presented in Appendix D as I I Frames <br />at a scale of 1:4,800. The dominant composition of each unit is provided along with general information <br />related to the topographic setting, inclusions, and recommended salvage depths. The recommended <br />salvage depths are preliminary and are based on the suitability criteria presented in the POS, field <br />observations, and an understanding of the probable variability based of the factors influencing pedogenesis <br />in the area. These depths and limiting characteristics should be further reviewed and evaluated in the <br />context of reclamation objectives following development of the mine plan. Soil map unit and plant <br />community correlations can be determined by comparing the results of this survey with the Collom <br />Mining Area Baseline Vegetation Survey prepared by Cedar Creek Associates (2006). <br />Soil Salvage Recommendations <br />The topsoil and subsoil horizons in the Survey Area exhibit the most alteration from the parent material <br />and are the substrates most suitable for use as plant growth media. The topsoil generally exhibits more <br />loamy textures, fewer coarse fragments, higher organic matter content, and higher nutrient <br />C concentrations than the subsoil and may warrant segregated salvage and storage where conditions permit. <br />Each of the soil pedon descriptions were reviewed to determine the optimum salvage depth at each <br />location. These depths were then used to identify the observed range and average salvage depth for each <br />of the soils in the Survey Area. These depths are provided in Appendix B, Table B-6. These <br />observations were further used to identify the probable depths of optimal topsoil and subsoil salvage in <br />each of the map units, as shown in Appendix B, Table B-5. <br />The primary physical properties limiting salvage include high clay content and high coarse fragment <br />content. Soils on the ridge tops, especially the Campspass series, have extremely high clay concentrations <br />in the subsoil that may warrant special consideration for reclamation planning. High percentages of coarse <br />fragments are generally uncommon in the intervals proposed for topsoil salvage. However, many series' <br />subsoils, especially those classified as skeletal, have high volumes of coarse fragment. While some of the <br />soils exhibit moderate susceptibility to water erosion and others exhibit high susceptibility to wind <br />erosion, these factors alone are not expected to significantly limit their use in reclamation. <br />The primary chemical property limiting salvage is nutrient content. Nutrient content is variable <br />throughout the Survey Area, but the pachic Mollisols in the southern portion of the Survey Area <br />exhibited the highest nutrient levels and other qualities that make them suitable as plant growth media. <br />Relative to soils from the swales, valleys, and plateaus in the middle and southern portion of the Survey <br />Area, soils in the aridic moisture regime and the northern valley bottoms have low nutrient content and <br />are also often less suitable at shallow depths. <br />Materials proposed for salvage in Appendix B, Tables B-5 and B-6 can be expected to promote <br />vegetative growth, hydrologic function, long-term nutrient cycling, and erosional stability in the reclaimed <br />landscape relative to deeper materials. However, the need for salvage to the maximum depth of available <br />material will depend on the reclamation plan and the suitability of re-graded spoil in the re-graded <br />landscapes. As such, the recommended depths may not be appropriate where more or less soil <br />replacement is required to reclaim disturbances. <br />• <br />Tetra Tech, Inc. 13
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