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Mr. Alex Schatz <br />March 30, 2007 <br />Page 4 of 7 <br />Fountain Creek, the model should be adjusted as appropriate and new predictive results should <br />be produced to reflect this. <br />The model was initially run to steady state without any pits in place and calibrated so that <br />the water table level in the alluvium was recharged by the river and the saturated thicknesses <br />agreed with those indicated in the site boring logs. These heads were then used as the starting <br />heads in the remaining model runs simulating pit dewatering. <br />Fountain Creek was modeled using MODFLOW's river package with the hydraulic <br />conductance of the riverbed set to 20,000 square feet per day in each river cell, and the river <br />bottom one foot below the head in the river, which ranged from an elevation of 5,330 feet at the <br />north end of the mode] to 5,250 feet at the south end of the model. Riverbed elevations were <br />based on USGS topographic maps. <br />Modeling of Pits <br />Based on information obtained from Lafarge, the gravel pits will be mined essentially to <br />bedrock, which is approximately 40 feet below ground surface. Consequently, the pits were <br />modeled with perimeter drains set at a depth approximately one foot above bedrock. This will <br />allow the cells to be dewatered to within approximately one to two feet of bedrock. The drain <br />hydraulic conductance was set to 50,000 square feet per day for each drain cell. <br />The mining cells were modeled one at a time in accordance with our current <br />understanding of Lafarge's plan to mine each cell individually. <br />1. Cell t was modeled with perimeter drains as the site reservoir in the northwest <br />portion of the site was modeled as an open body of water. <br />2. Cell 1 was then partially converted to a site reservoir (approximately 8 acres) and <br />silt pond (approximately 10 acres) while Cell 2 was modeled with perimeter <br />drains. The site reservoir and silt pond within Cell 1 were maintained for the <br />remainder of the modeling. <br />3. Cells 3 and 4 were then modeled individually each with perimeter drains. <br />4. Cells 5 and 6 were then inactivated because ground water flow will not be <br />allowed through the cells once the slurry walls are constructed around each cell. <br />A model run was performed to determine the shadow and mounding effects <br />associated with the slurry walls. <br />5. Cell 7 was then modeled with perimeter drains and with a recharge system that <br />extended along the western side of Cell 6, across the bottom of Cells 7 and 8, and <br />up the eastern side of Cell 8. <br />6. Cell 8 was then modeled with perimeter drains and a recharge system while Cell 7 <br />was modeled as an open body of water. <br />Areas modeled as reservoirs, silt ponds, or open bodies of water were assigned a specific <br />yield of 100 percent to simulate open bodies of water. The recharge system was adjusted so that <br />5:\536 -Banks and Gesso, LLC\536.4 - Sundance Pi[\Repori\Final Letter Report.doc <br />Martin and Wood Water Consultants, Inc. <br />~~ <br />-. - _ -._..:-c-. _~.~.~ ~- _ _ ---.. <br />