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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 />bedrock (carbonate cemented sedimentary materials) under an ustic regime in the central portion of the <br />Survey Area generally have the most neutral of all soils. <br />This correlation is reflective of three factors: <br />I) soils at higher elevations likely experience more leaching, which removes carbonates from the <br />soil and lowers pH; <br />2) The loess that influences many of the high elevation soils does not appear to have had a strong <br />carbonate component; <br />3) Soils in the northern portion of the Survey Area are in an aridic moisture regime that leads to <br />high carbonate accumulation at shallow depths. <br />The pH of all samples tested ranged from 5.6 to 8.8 and averaged 7.04. While this range is broad, it is <br />unlikely that pH is a significant limiting factor for use in reclamation, except where obvious accumulations <br />of carbonates (e.g., aridisols) are evident in the deep subsoil. <br />Electrical Conductivity <br />A soil's EC is a measure of the salt content of the soil (measured as mmhos/cm) and is directly related to <br />osmotic potentials and water availability. Soils with an EC less than 8.0 mmhos/cm are generally <br />considered non-limiting. Of the soils sampled in the Survey Area, only two samples exceeded this <br />threshold and almost all of the other samples were below 2.0 mmhos/cm. Those samples with the highest <br />EC, including those that exceeded 8.0 mmhos/cm, were taken deep in the profile (20 to 40 inches below <br />ground surface) of soils with high clay content (Cochetopa, Morapos, and Campspass). Often the high clay <br />content would make these soils unsuitable for salvage regardless of the conductivity. EC is not a notable <br />limiting factor in the Survey Area. <br />Sodium Adsorption Ratio <br />The SAR of the soil is a measure of soil sodicity, which degrades soil structure and inhibits plant growth at <br />C higher levels. Levels above 8.0 can be limiting and may cause surface crusting. Levels above 12 are further <br />limiting and may require treatments with amendments to revegetate. The SAR of most soil sampled was <br />less than 2.0 with only three exceeding 8.0 and none exceeding 12. All of the soils with an SAR over 8.0 <br />were taken from below 24 inches in the soil profiles. Most of the soils with the highest SAR (Cochetopa, <br />Campspass, and Yamo) were also observed to have high EC. These results indicate that SAR is not a <br />notable limiting factor in the Survey Area. <br />Nutrient Content <br />The nutrient content of native (non-cropland) soils is generally low, and therefore there are not strict <br />guidelines for determining limitations. However, data from the various series across the Survey Area <br />provided a reference base to compare within. Phosphorus content ranged from 0.03 to 34 milliequivalents <br />per liter (meq/L) and averaged six (meq/L). The soils with the lowest phosphorus levels were the Aridisols <br />(Forelle, Yamo, etc.) while the highest phosphorus levels were found in Lamphier, Campspass, and Weed <br />soils. Potassium levels ranged from 11.3 to 1430 (meq/L) and averaged 276 (meq/L). Potassium was found <br />at the highest levels in the Rhone, Lamphier, and Shawa series and lowest levels in the Danavore and <br />Yamo series. Available nitrogen levels ranged from 0.02 to 35.8 (average = 2.52) with the most nitrogen <br />available (on average) found in Rhone and similar soils. No series was especially low in nitrogen content. <br />Soil organic matter is a critical source of nutrients in native soils and often accounts for low free nutrient <br />levels. Soil organic matter ranged from to 0.3 to 9.6 percent and averaged 3.13 percent. The Aridisols and <br />Entisols exhibited the lowest organic matter content, while the pachic mollisols, Rhone, Lamphier, and <br />Cochetopa series had the highest content. <br />Boron and Selenium <br />Concerns over boron and selenium content in mine soils prompted testing of background levels in the <br />Survey Area. The soils tested revealed boron concentrations ranging from 0.07 to 1.34 parts per million <br />(ppm) and averaging 0.39 ppm. Selenium levels range from less than 0.02 to 1.0 ppm with most registering <br />below the detection limit. The WDEQ Topsoil and Overburden Guidelines specify recommended <br />Tetra Tech, Inc. 12
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