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Ms Mary Meays Page 2 <br /> April 13, 1994 <br /> confirmed after construction and development of monitoring wells at both sites <br /> • indicated that stabilized water levels tended to be higher than initial water levels <br /> In general, the ground water potentiometric surface at the site is at a depth of <br /> approximately 4 to 6 feet bgs <br /> Potentiometric surface maps prepared individually for Sites 1 and 2 between <br /> January 1991 and March 1993 have consistently shown ground water flow <br /> directions to be toward thesouth-southwest The predominant flow direction <br /> appears to be away from the Stockton Deep Water Channel, which lies <br /> immediately north of the property line Tidally-induced water level fluctuations <br /> in the channel appear to be the cause of slight-to-moderate variations in the <br /> ground water flow gradient <br /> Ground water wells are a common source of potable water in the Great Valley <br /> geomorphic province However, no water supply wells are located within a 2,000- <br /> foot radius of the West Weber sites <br /> PREVIOUS INVESTIGATIONS <br /> A brief summary of the ground water investigation activities previously <br /> conducted at Sites 1 and 2 is provided below (for additional details, see the <br /> Preliminary Assessment Report prepared by ERM-West in May 1993) For <br /> reference, see the attached General Site Plan illustrated in Figure 1 <br /> Site 1 1515 West Weber <br /> A release of petroleum products to ground water from a 2,000-gallon underground <br /> gasoline storage tank formerly located at Site 1 was documented Subsequent <br /> investigations conducted at the site defined the extent of the release The extent of <br /> total petroleum hydrocarbons (TPH) and benzene, toluene, ethylbenzene, and <br /> xylene (BTEX) in ground water was limited to a localized area in the vicinity of the <br /> former tank, and no significant migration of chemicals in ground water has been <br /> observed over time The results of quarterly ground water samples collected from <br /> the five site monitoring wells between April 1991 and April 1993 showed a steady <br /> decline in the concentrations of TPH as gasoline and benzene in ground water <br /> All monitoring wells at Site 1 (except for well MW-5) have been non-detect for <br /> these compounds since December 1992 MW-5 is located directly beneath the <br /> former tank <br /> Site 2 1325 West Weber <br /> A release of petroleum products to ground water from a 500-gallon underground <br /> gasoline storage tank formerly located at Site 2 was documented The extent of the <br /> release was defined during a Phase I and Phase II investigation The extent of TPH <br /> and BTEX in ground water at Site 2 was limited to a localized area surrounding <br /> monitoring well MW-1A (located lust north of the former tank location) Based <br /> . on historic ground water level data, MW-1A is upgradient of the former tank <br /> location The remainder of the monitoring wells at Site 2 (MW-2A through MW- <br />