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Mr. J.C. York <br />July 13, 2015 <br />Table 2 - Steady State Mass Balance Prior io Loloff Pit . <br />Parameter <br />Inflows (cfs) <br />Outflows <br />(cfs) <br />In - Out <br />(cfs) <br />River <br />2.2 <br />3.6 <br />-1.4 <br />Aquifer Subflow <br />5.6 <br />4.2 <br />1.4 <br />Tota I <br />7.8 <br />7.8 <br />0.0 <br />Page 5 <br />The net river gain of approximately 0.7 cfs per mile appears reasonable. We do not believe that <br />the pit slurry wall would significantly change the overall timing and location of historical river <br />gains. <br />Model Runs <br />We conducted two model runs to evaluate the hydrologic effects of installing a slurry wall <br />around the Loloff Pit. Run Lol SS6 was meant to simulate the water table before the water <br />table was disturbed by pit excavation. Figure 1 shows the resulting water table gradient where it <br />crosses the Poudre River and through the outline of the future pit area and slurry wall. <br />In run Lol_SS7, the model cells within the pit area are turned off to not allow aquifer flow <br />through the pit which simulates the effect of proposed slurry wall. Figure 2 is the contoured <br />difference between the Post -Pit Run (Lol_SS7) — the Pre -Pit Run (Lol SS6). Positive values on <br />the left side of the pit reflect mounding and negative values on the right side reflect lower water <br />levels in the "shadow" of the pit. The maximum change in water levels is +1- 2 feet. <br />Model Sensitivity <br />The model results are insensitive to differences in hydraulic conductivities (K) since mound <br />height is inversely proportional to K and aquifer inflow is directly proportional to K. Therefore, <br />since the aquifer gradient and thickness are constant, an increase in K will cause a proportional <br />increase in model inflows which would increase mound height proportionally, but this does not <br />occur because the higher K causes a proportional decline in mound build-up. <br />Model results are insensitive to streambed leakance since the streambed is very permeable so <br />large amounts of water can move in and out of the stream in response to up -gradient mounding <br />and the down -gradient shadow effect. The model is sensitive to the area of the slurry wall, but <br />this is a fixed parameter. Therefore, the model is relatively insensitive to input parameters and <br />boundary conditions. We believe however that the model results in Table 1 are sensitive to: 1) <br />the relative location of wells and vulnerable structures such as basements to the up -gradient side <br />of the pit; 2) to the accuracy of reported predevelopment water level depths; and 3) to the timing, <br />location, and magnitude of various types of recharge such as precipitation and canal recharge. <br />Model Results, Uncertainty, Mitigation, and Recommendations <br />Results, uncertainty, mitigation, and recommendations are discussed earlier in the report. <br />