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PERMFILE135227
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PERMFILE135227
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Entry Properties
Last modified
8/24/2016 10:35:58 PM
Creation date
11/26/2007 3:12:45 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981014
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Doc Name
TR-14
Section_Exhibit Name
EXHIBIT 15 Part 9
Media Type
D
Archive
No
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ACZ <br />• hfs. Cathy Bcgcj <br />January 14, 1992 <br />Page 2 <br />The proportional mix of coarse and fine refuse varies dependent oo changes in geologic and <br />mining conditions. <br />Given torten[ layered BII cons[ruuioa methods, the potential for arcular failure is signitican[ly <br />reduced and a sliding block failure through the fine refuse material may be the more critical <br />failure mechanism. <br />Actual strength testing of fine «fuse materials indicates a higher ctfcctive Crictioo angle, at the <br />densities documented by field sampling, than assumed far previous stability analyses. <br />2.0 Existing Conditions and Material Properties <br />The current refuse placement practice at the mine consists of a layered placement with the coarse and Cme <br />components being placed is individual layers. The fine refuse is considered to be a lower strength material than <br />the coarse refuse. The stability evaluation will, therefore, focus oa the fine refuse layers az the primary <br />structural units influencing overall stability. The presence of the coarse material in individual layers may be <br />an advantage, is that [hey will tend to alt as drainage layers for the fine refuse, intercepting and conducting <br />infiltration Bows to points oa the pile surface where these layers daylight. <br />• Figure 1 indicates the general geometry and layout of the refuse pile az of the end of 19g9 and it's planed final <br />coafiguratioo. Review of this figure indicates that the pile haz beta coastruaed with approximately 3H:1 V side <br />slopes to a maximum height of 80 feet Figure 2 indicates two uoss-seaioas through the pile [hat were taken <br />at critiral locations (steepest side slopes and highest overall slope). These sections indicate the extent of refuse <br />materials, the loratioa of underdrains, and the assumed subsurface stratigraphy. These two cross-sections were <br />used to conduct liability analyses of the refuse pile is it's current and planned final configuration. <br />The material properties used for the refuse and the foundation soils are presented is Table 1. Additional <br />testing (GeoWest, 19g8) focused oa measurement of in-place densities and included strength testing of fine <br />refuse materials. A series of direct shear tests were conducted oa the fine refuse materials recompacted to <br />varying densities. The results of the d'vcu shear tests indicated that [he friction angle varied from 33 degrees <br />to 38 degrees for recompaded densities of 45 to 63 pcf, respectively. <br />While the triaion angles determined by direct testing appear relatively high (or fine refuse, it should be noted <br />[hat EFCI designates fine refuse az any material smaller than ?$ mesh which is a medium sand. Shear test <br />results also appear to be consistent with Gthologic and tamtral charaaerizatioa of roof and Boor materials az <br />summarized by Table 4, Textural Analysis of Roof/Floor Material, Table 7, Jack O'I.antern Roof/Floor <br />Analyses (Parts 1 and 4), and Table g, Red Arrow Roof/Floor Analyses (Parts 1 and 4) of Southfield permit <br />document. These tables indicate that coal refuse materials are primarily saadstoau and shales with a « latively <br />high percentage of sand-sized particles and low clay content. Given the low rlay content, plastiaty is not a <br />significant coasideratioa and the friction angles indicated by testing are within the normal range for 28 mesh <br />granular fines. <br />The lower bound of the test values was chorea for the stability analyses. Material properties for the sandy clay <br />• material encountered at the original ground surface (foundation material) are based oa values reported by <br />Roclty Mountain Geotechnit:al, Inc 1982. <br />
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