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�C-- <br /> L <br /> D <br /> t <br /> ASS O C I ATE S I N C . <br /> reduce volatilization. Sample containers were then labeled with sample identification, placed on <br /> ice, and shipped under chain-of-custody to Sequoia Analytical. <br /> ' The groundwater samples from wells MWI, MW2, and MW3 were analyzed by Sequoia for <br /> TPHg, TPHd, TPHss, BTEX, and oxygenate fuel additives. Groundwater analytical results are <br /> summarized in Table 3, and laboratory data sheets are presented in Appendix F. <br /> 4.0 SUBSURFACE CONDITIONS <br /> ' Soils ingr oundwater monitoring wells MWI and MW2 from the surface to approximately 6.5 to <br /> 10 feet bgs consist of clayey sand. Soils from between 6.5 to 10 feet bgs and 11.5 to 15 feet bgs <br /> ' consist of lean clay. Soils from between 11.5 to 15 feet bgs and 21.5 to 25 feet bgs consist of <br /> elastic silt and varying amounts of poorly graded sand. Soils from between 21.5 to 25 feet bgs <br /> and 31.5 to 35 feet bgs consist of silt with sand and lean clay with sand. Soils from between 31.5 <br /> ' to 35 feet bgs and 36.5 to 40 feet bgs consist of elastic silt. Soils from 36.5 to 40 feet bgs and 43 <br /> feet bgs, the maximum depth explored in groundwater wells MMI and MW2, primarily consisted <br /> of lean to fat clay. Groundwater was encountered at approximately 26.5 feet bgs during drilling <br /> ' activities. <br /> Soils in boring SB2 from the surface to 40 feet bgs were not identified by lithology because this <br /> boring was advanced in approximately the same location as soil boring SB 1 and the soil lithology <br /> from the surface to 40 feet bgs was identified in boring SBI. Soils in boring SB2 from between <br /> ' 40 feet bgs and 41.5 to 45 feet bgs consist of lean clay. Soils from between 41.5 to 45 feet bgs <br /> and 51 to 55 feet bgs consist of sandy elastic silt. Soils from between 51 to 55 feet bgs and 67 <br /> feet bgs consist of fat and lean clay. Soils from between 67 feet bgs to 69.5 feet bgs consist of <br /> ' silty sand, clayey sand, and poorly graded sand. From 69.5 to 70 feet bgs, the maximum depth <br /> explored lean clay with sand was encountered. <br /> ' 5.0 ANALYTICAL RESULTS <br /> 5.1 Soil Analytical Results -Drilling Activities <br /> tSoil samples collected from borings MWI, MW2, and SB2 contained no detectable <br /> concentrations of BTEX or TPHss. TPHg and TPHd were detected at very low concentrations in <br /> tthe sample from boring MWI collected at 25.5 feet bgs. No detectable concentrations of TPHg <br /> and TPHd were detected in the remaining soil samples collected from borings MWI, MW2, or <br /> SB2. Analytical results of soil samples are summarized in Table 1. Laboratory data sheets and <br /> ' chain-of-custody documentation is presented in Appendix D. <br /> ' S�2 Groundwater Analytical Results <br /> Groundwater samples collected from wells MWI and MM2 contained no detectable <br /> concentrations of TPHg, TPHd, TPHss, BTEX, or oxygenate, fuel additives. Groundwater <br /> samples from wells MWI and MW2 contained 1,2-DCA at concentrations of 1.2 ppb and 2.0 ppb, <br /> W:17295 \s„rui.doc 5 <br /> 1 <br />