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2011-07-13_REPORT - C1981008 (9)
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2011-07-13_REPORT - C1981008 (9)
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Last modified
8/24/2016 4:35:38 PM
Creation date
7/13/2011 1:26:24 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981008
IBM Index Class Name
REPORT
Doc Date
7/13/2011
Doc Name
2010 Annual Reclamation Report
From
Western Fuels Colorado
To
DRMS
Permit Index Doc Type
Annual Reclamation Report
Email Name
MLT
SB1
Media Type
D
Archive
No
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analyzed for electrical conductivity by the paste method (EC), pH by the paste method (pH), sodium <br />adsorption ratio (SAR), and percent saturation. No exceedances of criteria listed n the permit Table <br />2.05.4(2)(d)-1 Spot inn/ Soil Suitability Criteria were noted. Laboratory results and chain-oretistody <br />!bins are a:lathed to this letter. Results are summarized in Tablet. <br />NOV S'tep 2 - This step required resampling die Bench 1 Subsoil Substitute Topsoil (formerly called <br />"suitable subsoil") sites on the Lloyd property, and analyzing the soil for saturation percent, SA.R, <br />CaCO3. selenium (Sc), and coarse fragments. Pits excavated by WPC at the previous sampling <br />locations were inspected by Walsh. Each pit was inspected by sweeping off a Dice of the pit, <br />measuring the depth of the pit and marking the 24-inch and 48-inch depths below the base of topsoil, <br />visually estimating the percent boulders, stones, and cobbles using USDA criteria in the 0-24 and 24- <br />48-inch depth %ones, and obtaining full-thickness soil samples from both depth intervals and placing <br />each into a graduated sieve with a 2-millimeter final sieve size, and sieving the soil into a bottom pan. <br />The volume percent of soil being caught in the 2-mm and larger sieves was estimated, the sieve pans <br />and excavation were photographed, and two samples of the less than 2 mm fraction were obtained <br />From each depth interval for laboratory analysis. No boulders (>25 inches) were observed in any soil <br />pit. All field data were recorded on field data sheets, copies of which are attached to this letter, <br />Samples were analyzed for selenium by Key Laboratories of Grand Junction, Colorado, and other <br />analytes by Servi-Tech Labs of Hastings, Nebraska, with the results recorded in Table 2. The total <br />percent rock fragments Criterion was exceeded at NESS-240A and NHSS-241A and 13, and the <br />aven,ge percent rock frownent criterion was exceeded. No other execedanecs of relevant criteria were <br />noted. <br />In addition, a sample orspoil from 48 inches to the pit bottom (between 55-82 inches) was obtained <br />from selected pits for analysis of boron, pH, and EC by Servi-Tech Labs, with results recorded on <br />Table 5. No exceedanees, of relevant criteria were measured at any sampling location. <br />NOV Step 3 This step involved re-sampling Bench I Subsoil Substitute Topsoil from the Morgan <br />properly at sample points SS-31 through SS-44. The 0-36 inch soil :ntervals at these points had <br />previously been inspected by Lambert and Associates. Inc. in May. 2010; however, they did not <br />determine coarse rock fragment percentages, nor did they report soil texture using USDA er'neria. <br />Walsh calculated gravel percentage from Lambert's grain size distribution curves and recorded. these <br />results in Table 3. and calculated soil texture based on Lambert's grain size distribution curves using. <br />USDA grain size criteria and texture criteria and recorded these results in Table 4. All textures found <br />were sLtitable <br />In addition, pits excavated by WFC at the previous sampling locations were inspected. Each pit was <br />inspected by sweeping off a face of the pit, measuring the depth of the pit and marking the 36-inch <br />depth below the base of topsoil, visually estimating the percent boulders, stones, and cobbles using <br />USDA criteria in the 0-36 and >36-inch depth zones, and obtaining a full-thickness soil sample from <br />the 0-36-ineh depth interval. In pits where observed gravel estimates varied from the Lambert report <br />(SS-32 and SS-34}, soil from the 0-36-inch interval was placed into a graduated sieve with a 2- <br />millimeter final sieve size, and sieved into a bonom pan. The volume percent of soil being eatntht in <br />the 2-mm and larger sieves was estimated, the sieve pans and excavation were photographed, and the <br />Valsh <br />F,rivo nmental Scientists and lirtgineers,LLC <br />
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