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Mr.Jeff Gregg (Lcf <br /> January 5,2006 <br /> Page 4 7 <br /> CIVIL RES'PURCES,LLC <br /> MATERIAL PROPERTIES <br /> Overburden <br /> The index properties for the insitu clay overburden were based on field testing data and on our engineering judgment; <br /> the following parameters have been used to model the overburden. <br /> Dry Unit Moist Unit Saturated Unit Cohesion C'psf Friction Angle�A'° <br /> —Weight(pcf) Weight(pcf) Weight cf <br /> 103 114 126 200 28 <br /> Alluvial Sand and Gravel <br /> The sand and gravel is generally medium grained sand,medium dense,poorly to well graded,and generally clean. The <br /> deposit ranges from fine to coarse sand with some silt and occasional rounded to well rounded gravels less than 2- <br /> inches in diameter. The alluvial sand and gravel has been modeled as follows: <br /> Dry Unit Moist Unit I Saturated Unit Cohesion C'psf Friction Angle 0'0 <br /> —Weight(pcf) I Weight(pcf) Weight c <br /> 119 1 129 1 130 A 0 35 <br /> Claystone Bedrock <br /> The proposed mine area is generally underlain by claystone bedrock. Claystone is generally a weak bedrock and is <br /> often prone to slope instability and the bedrock foundation strength is critical for the highwall stability. For the claystone <br /> bedrock,two potential strength conditions were considered. These strength conditions are referred to as: 1)peak <br /> strength,and 2)residual strength. <br /> Peak strength is the maximum shear strength the claystone bedrock exhibits. The shear strength is made up of both <br /> cohesion(diagenetic bonding)and internal friction. Under short-term conditions for unsheared claystone,peak strength <br /> governs behavior. If a sheared surface or sheared zone is present within claystone as a result of faulting,slippage <br /> between beds due to folding,past shrink-swell behavior,stress relief,or from a landslide,the cohesion along the <br /> sheared surface is reduced to zero,and the angle of internal friction is decreased,due to alignment of clay minerals <br /> parallel to the shear plane. Under these conditions a claystone exhibits its lowest strength known as residual strength. <br /> Residual strength bedrock occurs in discrete zones,parallel with the sheared surface or zone,whereas fully softened <br /> strength occurs over a broader area.Based on data from other recent jobs,and engineering judgment,we modeled the <br /> claystone as follows: <br /> Dry Unit Moist Unit Saturated Unit <br /> Weight(pcf? Weight(pcf) Weight(pcf) Cohesion C'psf Friction Angle�'° <br /> 116 124 134 Peak= 100 Peak=28 <br /> Residual=0 Residual= 15 <br /> Soil-Bentonite Slurry <br /> The proposed slurry wall will consist of a mix of the overburden clay and imported bentonite.The resulting mix will <br /> produce a non-Newtonian fluid with some shear strength characteristics based on a reduced friction angle of the <br /> overlying clay overburden. Based on engineering judgment,we modeled the slurry wall as follows: <br /> Dry Unit Moist Unit Saturated Unit <br /> Weight(pcf) Weight(pcf) Weight(pcf) Cohesion C'psf Friction Angle rD'° <br /> NA 110 122 0 26 <br />