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5. Nature of the Material Available for Road Backfill <br />During the Fall of 1993, samples of fill material were gathered <br />from the roads and the mine portal areas. At each sample area, <br />approximately 100 to 200 l bs . of material was gathered over roughly <br />1/2 acre, gathering some material from the surface and some from <br />digging with a shovel. In all cases, the material gathered was <br />representative of the material which would be used in backfilling. <br />All sample locations are shown on Exhibit 1. <br />All samples were sent to CTL Thompson in Denver for sieve analysis, <br />plasticity indexes, liquid limits, optimum moisture content, <br />maximum dry density and direct shear tests to determine the <br />cohesion and internal angle of friction of the material. All lab <br />test data is included in Appendix A. <br />Only the samples from Mine Roads #3, #4, #5 and #2 Mine Bin Pad are <br />considered for this report. The sample from the #2 Mine Bin Pad is <br />actually on the road to Mines #1 and #2 in the cut through the <br />Rollins Sandstone. <br />As can be seen from the analyses, the percent silt and clay of the <br />materials (passing No. 200 sieve) range from 7% to 17 %. This <br />demonstrates the lack of fines in much of the material. Also, the <br />low plasticity indexes, ranging from 6 to 11, confirm the lack of <br />appreciable clay in the material. For this reason, it is not likely <br />that the material will expand or contract to a large extent after <br />backfilling; therefore, consolidated swell tests have not been <br />performed. Slake d u r a b i l i t y tests were performed on the samples and <br />the results show that the material is not readily weathered and <br />does not exhibit much shrink swell potential. However, water <br />infiltration is very likely due to the coarse nature of the <br />material and this is accounted for in the slope stability analyses <br />through use of a pore pressure ratio. <br />The hard, durable and angular nature of the material with little <br />clay indicates that it should possess little cohesion but should <br />have relatively high internal angles of friction. The results of <br />the direct shear tests show this to be the case. These tests were <br />performed under the consolidated - undrained condition and the <br />samples were compacted to 90% of their maximum dry density prior to <br />testing. Only that material that passed the #4 sieve was tested in <br />the direct shear apparatus. Larger particles cannot be used. <br />Therefore, it must be considered that, for each test, a large <br />portion of the material is not being tested. This larger size <br />material will have large friction angles and very low cohesion. <br />9 <br />