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PROBLEM ASSESSMENT REPORT <br /> Moore Petrolem, Inc. <br /> 1399 E. Yosemite Avenue, Manteca, CA <br /> NGA Project No. 10-90-480 <br /> Page 15 <br /> Dream was used to model the effectiveness of a ground-water <br /> remediation system using well MW-lA as an extraction well. Input <br /> - parameters for Dream are shown in Table 6. <br /> TABLE 5 <br /> DREAM Input Parameters <br /> Pumping well MW-1A <br /> Pumping Rate 0.35 GPM <br /> Aquifer 63 gallons/day/foot <br /> Transmissivity <br /> j Natural Ground-Water 0.001 foot/foot <br /> Gradient <br /> Aquifer Thickness 15 feet <br /> Aquifer Porosity 0.10 (estimated) <br /> ` Examination of the table of drawdown generated by DREAM for a <br /> pumping rate of 0.35 gpna indicates that this pumping rate is could <br /> likely be maintained by the aquifer. Figure 8 shows ground water <br /> flowlines generated by DREAM for this ground--Mater remediation <br /> scenario. Examination of Figure 8 indicates that pumping MW-1A at <br /> a rate of 0.35 gpm should easily capture the interpreted extent of <br /> dissolved hydrocarbons and prevent further migration of the <br /> dissolved plume. <br /> Figure 9 is a contour map of ground-water travel times prodvged by <br /> pumping MW-1A. Figure 9 indicates that shows that the northernmost <br /> extent of the dissolved plume of hydrocarbons would reach MW-1A in <br /> less than 200 days, and the majority of the plume reaching MW-1A <br /> in 50-100 days. <br /> - Because 3f adsorption and desorption of hydrocarbon constituents <br /> by aquifer materials (particularly fine-grained sediments and <br /> organic material) , it is likely that petroleum constituents will <br /> --___migrate somewhat-slower_than ground water. _A_conservative estimate <br /> of the relative rate of movement of dissolved petroleum <br /> constituents compared to the rate of ground-water movement would <br /> probably be aratio of about 1.5 to 1.0 (i.e., }petroleum <br /> constituents will migrate 1.5 times slower than ground water) . <br />