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111wf }2,11561 1; <br /> J. H.KLEINFELDER Sc ASSOCIATES <br /> After eighteen hours of pumping, the water table was depressed <br /> 9 . 76 feet at pumping well MW-7, a total of 0.34 feet at MW-4 , and <br /> E3,. <br /> � , 0.20 feet at MW-1 . Aquifer Dumping test data are provided in <br /> Eµ4 Appendix D of this report. <br /> Drawdown data collected during the aquifer test was analyzed by <br /> M*+ <br /> i , graphical techniques to provide a value for transmissivity. <br /> � . Theis ' non-equilibrium well formula curve matching and Jacob's2 <br /> modified non-equilibrium formula graphic solutions were employed. <br /> The excellent curve fit of field data to the solution type-curve <br /> indicates the techniques are valid for the hydrogeologic regime <br /> i <br /> -, at Guild Winery. A transmissivity of approximately 20,000 <br /> gallons per day per foot (gpd/ft) was calculated.. Twenty <br /> i. <br /> thousand gpd/ft is a reasonable value for the aquifer material <br /> present at Guild Winery. (Groundwateri Freeze and Cherrys, 1979) <br /> i <br /> �. 19:531 10 <br />