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09/07/2004 14:41 20946`118 AGE STOCKTON PAGE 08/10 <br /> 07 ,lune 2001. <br /> AGE-NC Project No. 95-0103 <br /> Page 4 of 6 <br /> For the pumping tests conducted at vapor well. VE-6, the draw down data.collected in observation <br /> points Tl, T2, T3 and well MW-3 and vapor well VW-1 were used to determine the aquifer <br /> properties.The draw down data collectedin observation wells MW-1,MW-7,and vapor well VW-7 <br /> during the extraction from well MW-4,was also used to determine the aquifer properties. Ground <br /> water levels in observation wells within twice the aquifer thickness or less than 30 feet away <br /> appeared to be influenced with measurable draw--down during the pumping tests. <br /> Results of the aquifer ground water pumping test are summarized in Table l; a site plan depicting <br /> the inferred radius of influence during the 07 March 2001 pumping test is depicted in Figure 3. <br /> Sten Drawdown Test- 07 March 2001 <br /> Utilizing data collected from wells T1, T2, T3 and MW-3, transmissivity value was calculated at <br /> 131.25 W/day or 979.5 gallon/day/feet,a storativityvalue calculated at 0.08,a hydraulic conductivity <br /> value of 0.02 cm/s and a radius of influence projected at 35 feet utilizing a semi-logarithmic plot of <br /> draw-down versus distance(Appendix D). <br /> Constant Rate Dr7T4-down Tc°st - 12 Ildarch 2001 <br /> Utilizing data collected from well Tl,T2,T3 and MW-3,vapor well VW-1, a transmissivity value <br /> was calculated at 87.5 W/day or 653 gallon/day /feet, a storativity value calculated at 0.0325, a <br /> hydraulic conductivity value of 0.015 cm/s and a radius of influence projected at 55 feet utilizing a <br /> semi.-logarithmic plot of draw-down versus distance (Appendix D). <br /> Consl.ant Rate Dr-a_ down Test — 29 March 2001 <br /> Utilizing data collected from well MW-1,MW-7 and vapor well.VW-7, a transmissivity value was <br /> calculated at 140 ill/day or 1,045 gallon/day/feet,a storativity value calculated at 0.032,a hydraulic <br /> conductivity value of 0.015 cm/s and a.radius of influence projected at 70 feet utilizing a semi- <br /> logarithmic plot of draw-down versus distance(Appendix D). <br /> Results of the aquifer ground water pumping test are summarized in Table 1; a site plan depicting <br /> the inferred radius of influence during the 27 March 2001 pumping test is depicted in Figure 3. <br /> 3.3. PI.JRGFD GRotTND WATER DISPOSAL <br /> Advanced GenEnvironmentnl.Inc. <br />