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• <br />• <br />Murari P. Shrestha, P.E. <br />August 25, 2010 <br />Page 5 <br />distances utilized in the IDS AWAS analysis were measured from the centroids for each <br />mine site to the identified points of depletion, as presented in the attached Figure 1. For <br />New Horizon North, well pumping depletions will occur to Tuttle Draw below the Holder <br />Ditch and the Charlie Rice Ditch, as shown on Figures 2.A and 2.B. Return flows from <br />the septic system will return to Tuttle Draw, based on the understanding that the septic <br />system will be located near the southwest corner of the New Horizon North Mine area. <br />For the Cyprus Block area, depletions will occur to Calamity Draw north of the mine <br />area, and return flows occur to Calamity Draw slightly upstream of the point of depletion, <br />as presented in Figures 2.A and 2.B. Figure 2.B also shows locations where augmentation <br />deliveries can be made in accordance with Western Fuels' augmentation plan described <br />in the Water Solutions, LLC report. The Glover lagged depletion analysis simulated an <br />infinite aquifer for this analysis; boundary conditions other than the stream were not <br />simulated. <br />The equilibrium lagged depletions and accretions resulting from the operation of water <br />supply wells at the New Horizon North and Cyprus Block are presented in the attached <br />Table Nos. 3.A and 4.A and in the attached Figure Nos. 3.A and 4.A, respectively. As <br />expected, lagged net depletions for both locations occur throughout the year but are <br />greatest late in the irrigation season. Although the peak water use and return flows occurs <br />in the month of June, the peak lagged depletion and return flow occurs in the month of <br />August. We have also provided lagging factors for both depletions and return flows <br />which can be used for the purposes of a water balance or water rights accounting. The <br />lagging factors are presented in Table Nos. 3.B and 4.B and Figure Nos. 4.A and 4.B, <br />respectively. <br />Analysis of Timing Impacts of Dewatering Pumping <br />Western Fuels pumps dewatering water from the mine to an above ground tank, which <br />then drains to sediment control ponds, which then drain to surface streams. Water from <br />the tank is used to fill trucks which apply the water for dust control purposes. Based on <br />field investigations and information provided by Western Fuels, it appears that the water <br />pumped from the existing New Horizon mine is largely influenced by irrigation <br />operations up gradient of the mine. The water pumped from the pit is largely believed to <br />be irrigation return flow. Field observations completed near the end of the 2009 irrigation <br />season supported this claim based on inflow to the pit from near the surface, although it <br />was noted that inflows to the pit in lesser quantities were also discharging from bedrock <br />material as well. In order to validate this position, BBA reviewed pumping records from <br />the New Horizon Mine and compared them with reported irrigation diversions from the <br />CC Ditch, historically known as the Highline Canal (hereafter, "CC Ditch "). <br />A comparison of the timing of irrigation diversions in the CC Ditch and the timing of <br />pumping from the pit is presented in Table 5 and Figure 5. The peak pumping from the <br />pit occurs approximately three months later than the irrigation diversions. It is our <br />opinion that the difference in timing between the pumping in the pit and the irrigation <br />diversions indicates that the pit is effectively intercepting lagged irrigation return flows. <br />The lag of the irrigation return flows to the stream system would probably be slightly <br />greater if it were not for the presence of the mine pit. Effectively, the dewatering from the <br />pit delivers return flow water to the stream at a faster rate than it would otherwise occur, <br />www.bbawater.com <br />Bishop- Brogden Associates, Inc. <br />