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Linda J. Bassi April 29, 2008 <br />Page 4 <br />gradually until it reaches the actual rate of pumping. The hydrologic analysis using the <br />Glover approach was based upon the following data inputs: <br />Distance from well to Two Elk Creek: 120 feet <br />Distance from the aquifer no flow boundary to Two Elk Creek: 150 feet <br />Aquifer Hydraulic Conductivity: 150 feet per day <br />Aquifer Saturated Thickness: 50 feet <br />Aquifer Specific Yield: 0.2 <br />Under these assumptions, after well pumping is initiated, the impact on streamflows <br />would reach about 47% of the amount being pumped after 12 hours, and 72% with one <br />day X24 hours) of continuous pumping, as shown in Figure 2. When pumping is <br />terminated, however, any impact on streamflows in Two Elk Creek would begin to <br />diminish at approximately the same rate that occurred during pumping until the alluvial <br />aquifer fully recovers from the well pumping. When the aquifer fully recovers, the <br />streamflow would return to the natural pre-pumping flow. <br />While the impact of pumping at the rate of 15 gpm X0.033 cfs) is less than the 0.04 cfs <br />flow reduction that would typically be considered de minimis by the CWCB, the impact <br />on the actual flow would potentially be greater because winter flow conditions in Two Elk <br />Creek are considerably less than the 4.0 cfs ISF water right. This impact would be <br />mitigated through the delayed impact of well pumping on streamflows and the use of <br />intermittent rather than continuous pumping to reduce streamflow depletion rates. For <br />example, assuming well pumping fora 10 hour period, the impact on streamflow would <br />reach 57% of the amount being pumped after 3 days of pumping, as shown in Figure 3. <br />AMEC Earth and Environmental, Inc. <br />Figure 2. Hourly percentage impact of continuous pumping on streamflow. <br />