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' ESTER 1 GEOLOGIC RESOURCES , INC . <br /> J.Munoz/3 Apr 1989 4,. <br /> Ilk <br /> Since the three existing monitoring wells are only screened inJ the <br /> saturated zone, monitoring well MW-4, proposed in the 30 March 1988 report-' _ �'j 5 <br /> would also be partially screened in unsaturated material when instalIed`` <br /> Proposed remediation options for hydrocarbons remaining in the subsurface <br /> were outlined. <br /> 79 Jima 1988 - Gordon Boggs. RWOCB - CVR <br /> In a response to comments from the RWQCB - CVR, WA presented a workplan <br /> for additional subsurface investigation. The workplan was to address a <br /> revised location of monitoring well MW 4, which would be placed closer to <br /> the high concentration of hydrocarbons detected at the southwest corner <br /> of the excavation, and how further excavation would effectively remove <br /> soils containing hydrocarbons in both the unsaturated and saturated zones. <br /> The revised location of well MW-4 is presented in Figure 6. The well <br /> _ would be screened in unsaturated soils, if water-bearing sediments were <br /> - located above 25 ft below grade. A concern was expressed that low- <br /> permeability clays between 6 and 7 ft below grade may contain <br /> hydrocarbons, which could be carried down to groundwater, if the well was <br /> screened above the water-bearing zone. <br /> y The protocol for additional excavation included removal of all soil <br /> containing observable hydrocarbons to a depth of 23 to 24 in the southwest <br /> corner of the pit and analysis of 20% of samples collected from every 15- <br /> ft by 15-ft section of exposed wall . <br /> -0 <br /> 11 August 1988 - Julian Munoz. Safeway <br /> Betwe ,r2fi -and-28— Uy,WA--c-onducted_ 4d4itional excavation and soil <br /> sampling. One-hundred and fifty cubic yards of hydrocarbon-bearing soil <br /> were `removed half-way along the southern and western walls of the <br /> excavation to a depth of about 24 ft and stockpiled with the pea gravel . <br /> At that time, groundwater was at 23 ft in the monitoring wells. Soil <br /> samples TP-16 through TP-22 were collected from the floor and walls of the <br /> excavation and three composite pea gravel samples were also collected from <br /> the stockpile for analysis by Clayton Environmental Consultants (CEC) of <br /> Pleasanton, California. Soils collected from the excavation contained <br /> between less than 10 ppm to 3700 ppm TPH. Analytic results are presented <br /> in Table 1 . The pea gravel samples contained between 29 ppm to 180 ppm <br /> TPH. Analytic results are presented in Table 3. WA concluded that the <br /> highest concentrations of TPH occurred from about 15 ft below grade to a <br /> depth greater than previously determined and not defined by this <br /> investigation. <br /> 07611 ma9 <br /> C <br />