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KEI-P91-0202 .QR5 <br /> October 27 , 1993 <br /> Page 4 <br /> depth to ground water in the four monitoring wells varied from <br /> 49 . 83 to 52 . 86 feet below grade, and the direction of ground water <br /> flow was towards the northwest at a gradient of 0 . 02 . Analyses of <br /> the ground water samples collected from these wells yielded non- <br /> detectable results for TPH as gasoline and BTEX. Analysis of the <br /> soil samples from the borings for the wells indicated concentra- <br /> tions of TPH as gasoline and benzene ranging from non-detectable to <br /> 310 ppm and 0 . 29 ppm, respectively. <br /> The elevation of ground water at the Arco station is approximately <br /> 12 to 15 feet higher than at the Unocal site. The ground water <br /> elevations at the Arco and Unocal sites appear to be controlled by <br /> a low permeability clay unit, which most of the Arco and Unocal <br /> wells terminate within. This clay unit is present at the Arco site <br /> between 50 and 53 feet below grade, and at the Unocal site between <br /> 74 and 80 feet below grade. The elevation of ground water in the <br /> Arco and Unocal wells is generally within several feet of the upper <br /> contact of the clay unit. <br /> Based on the historical analytical and monitoring data for the Arco <br /> and Unocal sites, it does not appear that contamination from these <br /> sites has commingled. <br /> KEI has previously recommended that a meeting be held between both <br /> the San Joaquin County Department of Public Health and the RWQCB, <br /> to discuss the subsurface investigation that has been conducted at <br /> the Unocal site to date. As of the date of this report, Unocal has <br /> been unable to arrange a meeting. <br /> DISTRIBUTION <br /> A copy of this report should be sent to the San Joaquin County <br /> Public Health Services, and to the RWQCB, Central Valley Region. <br /> LIMITATIONS <br /> Environmental changes, either naturally-occurring or artificially- <br /> induced, may cause changes in ground water levels and flow paths, <br /> thereby changing the extent and concentration of any contaminants. <br /> Our studies assume that the field and laboratory data are reason- <br /> ably representative of the site as a whole, and assume that subsur- <br /> face conditions are reasonably conducive to interpolation and <br /> extrapolation. <br /> The results of this study are based on the data obtained from the <br /> field and laboratory analyses obtained from a state-certified <br />. laboratory. We have analyzed these data using what we believe to <br /> be currently applicable engineering techniques and principles in <br />