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�l <br /> 1 <br /> 1 <br /> 3330 Data Dnve <br /> Delta <br /> Suite 144 <br /> Rancho Cordova CA 95670 <br /> Environmental 91638 2085 <br /> Consultants,Inc FAX 916/638 8385 <br /> July 29, 1992 C �n 't 1 .t <br /> `- ��a <br /> AUG 0 9592 <br /> Mr Kenneth Earnest ENVIRONMENM HF-WH <br /> Ultramar Inc PERMIT/SERVIC S <br /> 525 West Third Street <br /> Hanford, California 93230 <br /> Subject Quarterly Monitoring Report, Second Quarter 1992 <br /> Beacon Station No 695 <br /> 900 South Cherokee Lane, Lodi, California <br /> Delta Project No 40-91-831 <br /> Dear Mr Earnest <br /> Delta Environmental Consultants, Inc (Delta), has been authorized by Ultramar Inc (Ultramar) to <br /> conduct quarterly ground water monitoring at Beacon Station No 695 located at 900 South Cherokee <br /> Lane, San Joaquin County, Lodi, California (Figures 1 and 2) This letter report contains the results <br /> of the quarterly ground water monitoring performed at the site on June 17, 1992 Field work <br /> conducted at the site by Delta was performed in accordance with the field methods and procedures <br /> described in Enclosure A <br /> Ground Water Levels, Flow Direction, and Hydraulic Gradient <br /> A total of 23 ground water monitoring wells are present at the site Monitoring wells MW-1, <br /> MW-16, MW-17, MW-18, MW-20, MW-21, MW-22, MW-24, MW-25, MW-27 and recovery well <br /> RW-1, contained measurable ground water on June 17, 1992 Ground water was not present in the <br /> other wells at the site The depth to ground water ranged from approximately 65 to 69 feet below <br /> the top of the well casings Ground water table levels in the monitoring wells have decreased <br /> approximately I foot since the previous monitoring event in March 1992 A summary of ground <br /> water levels recorded at the site since June 1991 is mLluded in Table 1 Enclosure B contains ground <br /> water level data since January 1988 <br /> The ground water level data recorded on June 17, 1992, were used to construct the water table <br /> contour map included as Figure 3 The water table contours indicate the inferred direction of ground <br /> water flow across the site was toward the southwest with an average hydraulic gradient of 0 02 A <br /> ground water mound in the vicinity of monitoring well MW-1 is probably due to the soil vapor <br /> extraction system at the site which was in operation during the measurement of ground water levels <br /> The system applies a vacuum to monitoring wells MW-1, MW-2, MW-5, MW-7, MW-8, MW-9, <br /> MW-10, MW-16, MW-17, MW-22, and MW-27 Previous ground water level data have indicated <br /> that the ground water flow direction at the site is toward the south or southwest The depth to water <br /> in monitoring well MW-22 (57 68 feet) on June 17, 1992, is not considered to be representative of <br /> ground water conditions at the site, therefore, this datum was not included in Figure 3 The total <br /> depth of monitoring well MW-22 is approximately 59 teet below grade and ground water was not <br /> present in any other wells at less than approximately 65 tees below grade The water present in <br /> monitoring well MW-22 was probably condensate trom moisture drawn into the well by the soil <br /> vapor extraction system <br /> Delta Delvers Solutions <br />