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i <br /> Canepa's Car Wash <br /> 248 E Park Street, Stockton, California <br /> aka. 642 N. Hunter Street <br /> Phase HSite Characterization and July 2, 1994 <br /> Quarterly Groundwater Report(May 1994) Page: 6 <br /> laboratory Care was taken to ensure that no air space existed in the vials by <br /> Iinverting to check for bubbles and re-sampling as necessary <br /> The samples were analyzed or extracted within 14 days according to their EPA <br /> methods Water samples collected for analysis were analyzed by EPA method 602. <br /> for BTX&E compounds, method 5030/modified 8015 for gasoline range <br /> hydrocarbons, and method 3 510 for diesel range hydrocarbons The muumum <br />' detection limits used for each analyte were 0 5 u&g for BTX&E, 0 5 mg/l for <br /> gasoline, and 0 05 mg/kg for diesel Analyses were conducted by Geo-Morutor of <br /> Hesperia, California, a State certified laboratory <br /> 4.0 Soil Conditions <br />' This site, at 248 E Park Street, Stockton, California, is located in the northern end of <br /> California's San Joaquin Valley This area is monotonous geologically, representing <br /> primarily, the alluvial flood and delta plains of the major rivers and tributaries of the <br /> region The region persisted as a lowland or shallow marine embayment during the entire <br /> Cenozoic period The surface of the Valley is composed of unconsolidated Quaternary <br /> sediments <br /> The Soil Survey completed in 1988 by the U S Department of Agriculture, Soil <br />' Conservation Service, generally classify the soil types as being Jacktone, HoIlenbeck or <br /> Stockton types Generally, these soils are somewhat poorly to moderately well-drained, <br /> fine texture soils that are moderately deep to deep, down to a cemented hardpan <br />' The hthologic units encountered in these bonngs were interbedded inorganic micaceous <br /> clayey silts and silty clays with numerous sands and silty, clayey sands of varying <br />' thicknesses This is typical of the valley fill deposits in the region <br /> Analysis of soil samples show B-1, 2 & 5 to have the lughest levels of contamination, <br />' while B- 3 & 6 and MW-1 & 2 had significantly lower levels Boring B-3 and MW-3 are <br /> approaching the lateral limits of contamination B-4 was the only boring that analyzed <br /> non-detect for all tested compounds Analyses of soil samples from MW4, 5, 6 and 7 <br />' define the lateral limit of soil contamination, with the exception of a thin sand lens at 25 <br /> feet in MW-6 (Figures 9 & 11, Table 1, Appendix A) <br /> 1 <br />