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Addendum to the Well Installation and <br /> Hydraulic Testing Report and Additional <br /> ARCADIS Well Installation Work Plan <br /> Former Occidental Chemical Corporation <br /> Lathrop, California <br /> was then increased in 5-gpm increments until the extraction rate was approximately 65 gpm. <br /> Groundwater extraction continued at 65 gpm for approximately 12 hours; however, groundwater <br /> elevations did not stabilize and continued to decline.The extraction rate was then reduced to 30 gpm. <br /> Groundwater elevations quickly stabilized in the observation wells at the 30 gpm extraction rate.After <br /> maintaining an extraction rate of 30 gpm for approximately three hours,the extraction pump was turned <br /> off and the aquifer was allowed to recharge. <br /> Calculation of Transmissivity. Storativity, Hydraulic Conductivity, and Radius of Influence <br /> The drawdown characteristics measured during the pumping test were used to estimate several <br /> hydrogeologic parameters of the water table zone, including transmissivity, storativity, and hydraulic <br /> conductivity. In addition, a radius of influence was estimated for extraction well EW-09. Several <br /> methods are available to calculate these parameters.A variation of the Jacob method, known as the <br /> Distance-Drawdown Method,was chosen based on the field data (e.g., Sutch and Dirth, 2003). <br /> Drawdown at the three observation wells(PW27-40, PW28-40, and PW29-40)was measured <br /> simultaneously while extracting from EW-09 at a constant pumping rate of 65 gpm.The observed <br /> drawdown in PW27-40 located 15 ft north of the pumping well was 6.89 ft.The drawdown in PW28-40 <br /> located 20 ft south of the pumping well was 6.70 ft and drawdown in PW29-40 located 30 ft north of the <br /> pumping well was 5.71 ft.Transmissivity was calculated using the following equation (Sutch and Dirth, <br /> 2003): <br /> T=70`Q/ds (Equation 1) <br /> where <br /> Q = Groundwater extraction rate in gpm, equal to 65 gpm <br /> ds= Drawdown per log-cycle of distance, i.e., measured as 7.7-3.7=4 ft, using Figure 4. <br /> T = Transmissivity, in ft2/day <br /> The hydraulic conductivity was calculated using the following equation: <br /> K=T/b (Equation 2) <br /> where <br /> T = Transmissivity, in ft2/day, calculated to be 1137.5 ft2/day using Equation 1 <br /> 2012-0913 addendum well Install work plan_hy test rpt.docx 3 <br />