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W1C]rR <br /> • Southwest, Inc. <br /> however, this detection may be indicative of an onsite source of TPH-g, which would be <br /> consistent with historical site usage. SWPPP maps show motor blocks have historically been <br /> stored near the location of B-2 (Hugo Neu& Sons, 1992 and The Learner Company, 1997). <br /> The three monitoring wells installed on the Learner site in 2002 following removal of the UST <br /> were located in the vicinities of B-8,B-11 and B-12. The wells were monitored quarterly during <br /> 2003, and during this time TPH-d was detected in all of the wells during all four quarters <br /> (Clayton Group Services, 2004). The highest TPH-d levels were consistently found in the well <br /> located near B-8, west of the hazardous materials container storage area. During this Phase II <br /> ESA, the highest dissolved TPH-d concentration was detected in the groundwater sample from <br /> B-8. Documented TPH-d contamination to groundwater remained when monitoring of the site <br /> was discontinued and the UST case was closed by the agencies in 2004. Detectable soil <br /> concentrations of TPH-d and TPH-g were also documented to have been left in place and may <br /> be contributing to soil and/or groundwater concentrations detected during this Phase II ESA. <br /> Widespread concentrations of TPH-d and TPH-mo in groundwater beneath the site may also <br /> be indicative of the long history of the site which has included auto shredding, onsite fueling, <br /> • vehicle and equipment maintenance and storage of a variety of petroleum products, as <br /> identified in the SPPCP. Learner has also stored and processed an extensive variety of metal <br /> products, including engine blocks from diesel trucks. The TPH-d and TPH-mo <br /> chromatograms typically show no recognizable pattern which is consistent with multiple <br /> sources and ages of petroleum hydrocarbons. <br /> The concentrations of TPH-d and TPH-mo in groundwater samples correlate somewhat with <br /> TPH-d and TPH-mo concentrations in one-foot soil samples (see Figure 4). Variations may <br /> be attributable to an array of factors including apparent multiple ages and sources of TPH <br /> releases, preferential pathways through coarser-grained subsurface soils and fluctuations in <br /> groundwater flow direction over time. <br /> It is not possible to compare the CAM17 metal analyses of groundwater samples from B-1 <br /> through B-7 with B-8 through B-18, since the former samples were not filtered and contained <br /> sediments. They provide a measurement of the total concentration of metals in the water <br /> samples, including dissolved and particulate metals. The latter samples were filtered and thus <br /> reflect only the dissolved metal components. Comparison of the dissolved metal <br /> concentrations from B-8 through B-18 to MCLS shows them all to be below MCL standards. <br /> • <br /> 704. PRI.05 27 July 21, 2008 <br />