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- Y <br /> .October4, 1994 <br /> : :Page 2 _ <br /> The site lies at an approximate elevation of 10 feet above mean sea level. The <br /> topography in the vicinity is essentially flat with a gentle'slope to the west toward <br /> the San Joaquin River, which is located 3 miles west of the site. <br /> The site is currently a vacant lot. Unocal originally leased the site in January 1947. <br /> The station was completely remodeled in 1967. The station was demolished <br /> . between February and April 1988. During station demolition, two 10,000-gallon <br />` underground gasoline tanks were removed from a common excavation along with a <br /> separate 550-gallon waste oil tank_ The former tank locations, along with the <br /> product islands and station building, are shown on Figure 2. <br /> During tank removal, 1,100 cubic yards of soil were removed from the site.`Soils <br /> 'within the tank excavation were removed to a depth of 30 feet. Soils at the-base of <br /> the excavation contained a maximum of 18 parts per million(ppm) total petroleum <br /> hydrocarbons calculated as gasoline (TPH-g) and 1.7 ppm benzene. Soils beneath <br /> the product lines were found to have a maximum TPH-g concentration of 6 ppm. <br /> No benzene was detected in the product line samples. No hydrocarbons were <br /> detected beneath the waste oil tank. <br /> Kleinfelder, Inc. installed five soil borings (K31,through KB5) at the site in <br /> January 1988. These-borings were installed around the former tank complex,adja- <br /> cent <br /> adja <br /> cent to the product islands-, and adjacent to the former waste oil tank (Figure 2). <br /> Between June 1988 and February 1992, Resna Industries, Inc. (Resna) installed a <br /> total of seven monitoring wells (MW-1 through MW-7) and three soil vapor extrac- <br /> tion (SVE) wells (VW-1 through VW-3). Resna also installed 11 soil borings (B-1 <br /> : .through B-11). Most of these borings were converted to either groundwater <br /> : .monitoring wells or SVE wells. The existing monitoring well and SVE well <br /> locations are shown on Figure 2. <br /> A SVE test was performed in March 1992 by.Resna. The results of this test show <br /> t: that with a w <br /> . ellhead flow rate of 43 cubic feet per minute cfm and an effectivedive <br /> P ( )� e <br /> f <br /> i radiuso influence of approximately 25 feet can be achieved for one vapor ex' <br /> trac-_ <br /> ` tion well. These results were documented in a report by Resna dated January 4,; <br /> 1993. <br /> All site groundwater monitoring wells are currently being monitored and sampled <br /> on a quarterly schedule. <br /> Soil Conditions <br /> The site is underlain by primarily fine-grained deposits consisting of interlayered <br /> clays and silts to an approximate depth of 50 feet.. Some surficial silty sands occur , <br /> to a depth of approximately 25 feet. Occasional interlaye red silty sands (up to <br /> :50 feet thick) were found to the total depth explored. . <br /> 31004002/MWINSTAL <br /> L <br />