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Ms. Margaret Lagorio,SJCEHD February 2,2009 <br /> Work Plan for Collection of Soil Gas Data <br /> Joe's Travel Plaza, 15600 S.Harlan Road <br /> Lathrop,California <br /> Page 2 <br /> According to Mr. Dhoot, the subject site has operated as a motor fuel dispensing facility since <br /> 1954. Several generations of underground storage tanks (USTs) and aboveground storage tanks <br /> (ASTs) have been installed at the site during the subsequent years. Currently, there are three <br /> gasoline USTs (12,000, 10,000, and 4,000 gallons) and one diesel UST (4,000 gallons) that <br /> supply the automobile dispenser islands, and four 10,000-gallon diesel ASTs that supply the <br /> heavy truck dispensers. The current station configuration is shown on Figure 2. <br /> BREIF SUMMARY OF PREVIOUS ENVIRONMENTAL WORK <br /> Environmental investigations at the site began in January 1997, when petroleum-hydrocarbon <br /> impact was identified during removal and replacement of USTs. Since that time, more than sixty <br /> (60) vertical soil borings have been drilled at the property and in surrounding areas to evaluate <br /> the lateral and vertical extent of soil and groundwater impact beneath the site. Of these borings, <br /> twenty-two borings were converted to permanent groundwater monitoring wells screened across <br /> three intervals of water-bearing strata beneath the site. Evaluation of potential remedial <br /> alternatives for the site (in the form of dual-phase extraction [DPE] pilot testing and groundwater <br /> pump testing) was performed at the site in June 2004 and December 2005. Quarterly <br /> groundwater monitoring and sampling was initiated in February 2000; and is currently ongoing. <br /> A summary of well construction details is included as Table 1. Historical groundwater <br /> monitoring and sampling data are included as Tables 2 and 3. <br /> GEOLOGY <br /> Based on available historic soil boring logs, soil beneath the site and surrounding areas is generally <br /> fine-grained (predominantly silty clays, clayey silts, and clays, and minor intervals of silts, sandy <br /> silts, and material classified by cone penetration test [CPT] as "stiff fine grained") to the total depth <br /> explored of 100 feet below ground surface(bgs). Three laterally extensive sand strata(identified as <br /> Sands A, B, and C herein) have been encountered within the fine-grained sequence, along with <br /> several thin laterally restricted sand bodies. Sand A is encountered approximately 5 to 8 feet bgs, <br /> and is approximately 3 to 10 feet thick. Sand B is encountered at depths between 25 and 35 feet <br /> bgs, and is approximately 7 to 18 feet thick. Sand B appears to extend north to south across the <br /> entire site vicinity, but may be limited laterally to the southwest. Sand C is encountered at depths <br /> between 50 and 65 feet bgs, and is approximately 15 to >25 feet thick. Geologic cross-sections <br /> illustrating interpreted stratigraphic relationships beneath the site vicinity are included as Figures 3 <br /> and 4. <br /> HYDROGEOLOGY <br /> Fifteen groundwater monitoring wells (MW-1 through MW-7, MW-9, MW-10, MW-11, <br /> MW-14A, MW-15A, MWO-1, MWO-2, MWO-3) have been screened to depths of about 20 feet <br /> bgs to monitor groundwater occurrence and quality in Sand A. In addition, one well <br /> K:Uoe's Truck Plaza\Work Plans\Work Plan for Collection of Soil Gas Data 2-2-09.doc <br />