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J&L Market • - 3 - • 8 May 2013 <br /> 8125 S. EI Dorado St., French Camp <br /> San Joaquin County <br /> significantly and full scale ozone remediation was not implemented. However during the last <br /> scheduled monitoring event in June 2011, eighteen months after the ozone pilot study, <br /> groundwater concentrations increased significantly at JLM5 (north of the station building) to <br /> levels approaching the pre-remediation levels of 2009 at JLM13. Additional groundwater <br /> monitoring was conducted to determine if a new USTs release had occurred. By March 2012, <br /> there was no evidence of a new release (included reviews of inventory reconciliation and USTs <br /> system sensor logs, and no reported drive-off spill) as concentrations were declining in JLM5 <br /> over two sampling events. The June 2011 spike in groundwater concentrations was attributed <br /> to groundwater rising and contacting residual soil contamination present at 20' bgs under the <br /> station building, due to the extremely wet 2010/2011 winter that caused water levels to rise <br /> onsite to the highest water levels recorded since groundwater monitoring began in 2002. Also <br /> note that monitoring well JLM5 is actually much closer to the station building than depicted in <br /> Figure 3, and the over-excavation to 30' below ground surface (bgs) was above the water table <br /> in 1995. Groundwater monitoring was suspended in March 2012 with staff concurrence, <br /> pending submittal of closure documents. <br /> Risk Assessment <br /> Two soil results (Figure 2) for TPHg (over-excavation confirmation sample P-15, <br /> 4,200 mg/kg west wall of excavation at 12.5' bgs, and the 2001 boring JLM2, 1,300 mg/kg at <br /> 20' bgs, Figure 2), taken in November 1995 and November 2001, respectively, exceeded the <br /> San Francisco Bay Regional Board Environmental Screening Levels (ESLs) for gross <br /> contamination and direct contact. P-15 and JLM2 were located below typical construction <br /> worker exposure depth. In February 2003, weathered TPHg was detected at JLM9 (8.2 mg/kg <br /> at 17' bgs) in a slanted boring under the station building. <br /> Even though the station is an active fueling facility that is exempt from a vapor intrusion <br /> evaluation under the low risk closure policy (LTCP), a soil gas survey was not required for <br /> closure, prior to implementation of the LTCP. Based on nearly 18 years since over-excavation <br /> removed the majority of soil contamination down to 30' bgs, with the depth to groundwater in <br /> excess of 20' bgs, and with the open bay construction of the station, there is a low threat of <br /> potential vapor intrusion due to residual soil and groundwater contamination. <br /> The groundwater plume is well defined both vertically and laterally (Figure 13). The plume is <br /> stable and has remained onsite, TPHg and BTEX have significantly declined at JLM5, and <br /> 1 , 2-DCA is declining very slowly at JLM13. Nearby domestic and irrigation supply wells are not <br /> threatened by the release. Groundwater concentrations will continue to decline, with Water <br /> Quality Goals estimated to be reached in 28 years. <br /> Sensitive Receptor Survey <br /> A 2011 sensitive receptor survey (ATC Figures 4 and 5, and Table 3) identified approximately <br /> 48 domestic supply wells and 5 public supply wells located within 2,000' of the Site. The four <br /> nearest wells are 200' to the northeast (domestic) and the southeast (domestic), and 400' to the <br /> north (irrigation) and to the east-northeast (domestic) of the Site. None of the wells are <br /> threatened by the petroleum hydrocarbons release at this Site. <br />