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REFUSE PILE EXPANSION <br />condition factor of safety is 1.22 during Sub-phase 1 B <br />along Profile 3. <br />• 5.5.3.2 Regional Stability of Entire Hillside <br />coefficient of 0.1 was included in the calculations to <br />account for a possible earthquake event. <br />5.5.3.3 Stability of RPE Pond and Highway <br />133 <br />A stratigraphic cross section alone the steepest <br />topographic gradient of the RPE was developed to <br />check the regional slope stability. The cross section <br />also included a profile representing [he maximum <br />thickness of the coal refuse which will occur at the <br />end of Phase IV construction. The stratigraphic <br />sequence of the RPE area was developed primarily <br />from li[hologic descriptions from three exploratory <br />wells drilled in September, 1996, in the vicinity of <br />the proposed RPE. In addition, six shallow auger <br />holes, drilled in April, 1996, were used to define the <br />colluvial and alluvial soil thickness along the slope <br />base. Figure E-1 shows the locations of the borings <br />and Appendix E contains the drilling logs. Well <br />data from the three exploratory holes were projected <br />along strike to align with the cross section shown on <br />Figure K-7. Bedding dips toward the north- <br />northeast at approximately 3.5 degrees. Field <br />mapping of sandstone outcrops agreed with the <br />projection of the sandstone stratigraphic layers. <br />Bedrock lithology includes shale, sandstone, and <br />coal from the Mesa Verde Formation underlying <br />varying thicknesses of colluvial and alluvial soils. <br />Well logs indicate competent, continuous bedding, <br />with the exception of some minor coal seams <br />feathered within larger carbonaceous shale layers. <br />For modeling purposes, the minor coal seams were <br />made part of the larger, weaker shale layers. Soil <br />strengths assigned to the strata are based upon <br />samples taken from the RPE site and are provided in <br />Table 7. The strengths and densities are based upon <br />geotechnical testing performed by RockTech <br />(October, 1996); corresponding geotechnical <br />analytical results are presented in Appendix K <br />The stability analysis was performed using the <br />SLOPE/W (Version 3) software produced by GEO- <br />SLOPE International Ltd., Calgary, Alberta, <br />Canada. The most likely catastrophic failure <br />scenario involving the entire RPE mass would occur <br />on a slip plane located along the base of the <br />colluvium and alluvium. Results, provided in <br />Appendix K, indicate construction of the RPE will <br />• ;effectively improve the stability of the slope as <br />shown in Table 8. A seismic acceleration <br />An additional slope stability analysis evaluated the <br />current Highway 133 conditions for the road fill <br />above the culvert draining [he wetland. At present, <br />minor soil erosion has occurred in this area. The <br />construction of the proposed RPE sediment control <br />pond will utilize this slope. The stability analysis <br />indicated a factor cf safety for the road fill to be 1.91 <br />for present conditions and 1.70 for earthquake <br />loading factors. <br />6.0 SURFACE HYDROLOGY <br />6.1 Introduction <br />A surface hydrology analysis was performed to size <br />the sediment pond, sediment ditches, and upland <br />runoff diversion (clear water) ditches required for <br />the RPE area during each of the four phases. <br />Peak discharges and maximum runoff computations <br />used in the design and size verification of all ditches <br />and sedimentation ponds were based upon <br />procedures from the following: <br />Urban Hvdroloev for Small Watersheds, <br />Technical Release No. 55, Soil Conservation <br />Service, U.S. Department of Agriculture, <br />January, 1975 <br />Procedures for Determining Peak Flows in <br />Colorado, TR-5> Supplement, Soil <br />Conservation Service, U.S. Department of <br />Agriculture, March. 1990 <br />HEC-1 Flood Hvdroeraph Package Computer <br />Program, U.S. Army Corps of Engineers <br />Hydrologic Engineering Center, Davis, <br />California, 1991 Revision <br />All ditches and diversions were designed to <br />accommodate the peak discharge from a 100-year, <br />24-hour, type II distribution, precipitation event <br />with an adequate freeboard of 0.3 feet. A v-notch <br />channel design was used for all ditches. Because of <br />Harding Lawson Associates 11 <br />