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December 1986 5 863-2060 <br />• <br />• <br /> <br />3.0 LABORATORY TESTING <br />Historic mine data are available which describe the geotechnical <br />properties of mine spoil and Mesaverde bedrock samples obtained <br />from Area 51, which is located immediately north of Area 9/10. <br />Because of the similarity of materials sampled in Area 51 and <br />Area 9/10, the geotechnical properties of the analogous materials <br />in the two areas are inferred to be similar. Gradation curves <br />for two Area 9110 mine spoil samples tested (ASTM D422) are pre- <br />sented as Figures 9 and 10. Pertinent Area 51 laboratory test <br />data are presented in Appendix B. <br />The Area 9/10 spoil samples tested are characterized as a well- <br />graded gravel with little to some sand, silt, and clay and <br />abundant cobbles and boulders composed of sandstone, siltstone, <br />and claystone fragments. Laboratory testing of Area 51 spoil <br />materials indicates similar gradation and composition. As shown <br />in Appendix B, consolidated, undrained triaxial compression test <br />data are available for Area 51 bulk spoil materials. Such test- <br />ing indicates that mine spoil has an effective friction angle (~) <br />of 33 degrees and a cohesion (C) of 300 psf. <br />Direct shear test data are available for a core specimen obtained <br />from the shale that underlies the Wadge coal seam in Area 51. <br />The testing was performed on a natural bedding plane joint in the <br />rock to .simulate the worst-case condition of sliding along a <br />plane of weakness. It indicates that appropriate strength param- <br />eters for this case are ¢ = 25 degrees and C = 1,400 psf. <br />In addition, historic mine dat <br />Atterberg limits, and uniaxial <br />samples collected from Area 51. <br />Appendix B. <br />a include moisture content, <br />compression test results for <br />These data are tabulated in <br />Golder Associates <br />