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REMEDIAL ACTION PLAN <br /> 1605 South EI Dorado Street.Stocidon California <br /> 3.0 SITE CHARACTERIZATION <br /> The following sections summarize the characterization of soil and groundwater <br /> 3.1 Soil <br /> Soil has been characterized during four phases of work at this site, three phases of <br /> drilling and one phase of UST removal These phases of investigation have assessed the <br /> magnitude and extent of petroleum hydrocarbon impact in soils beneath the site The <br /> locations of soil borings, groundwater monitoring wells, and vapor extraction wells are <br /> shown on Figures 4, 5, and 7 Analytical results from the soil boring samples are <br /> included in Tables 1 through 4 <br /> Figure 6 is a cross-section location map Interpretation of the subsurface is shown on <br /> geologic cross-section A-A' (Figure 7) The generalized cross-section indicates the soils <br /> beneath the site consist mostly of silty clay and clayey silts, with a relatively continuous, <br /> 5 to 10-foot thick silty to clayey sand layer extending from approximately 25-30 to 35 feet <br /> bgs The cross-sections include analytical results from samples collected during <br /> installation of the borings and the screened intervals of the vapor extraction wells and the <br /> groundwater monitoring wells <br /> As shown on Figures 4, 5, and 7, petroleum hydrocarbon impact under the site is <br /> primarily beneath the former UST near VEW-1 and VEW-2 at depths from 10 5 to 35 5 <br /> feet bgs <br /> 3 2 Groundwater <br /> There are currently five groundwater monitoring wells on-site (MW-1 through MW-5) and <br /> two additional off-site wells (MW-6 and MW-7) The most recent quarterly monitoring and <br /> sampling event (8/24/93) shows that groundwater was encountered at depths ranging <br /> from 42 47 to 45 06 feet bgs Groundwater levels collected to date are summarized in <br /> Table 5 A groundwater elevation hydrograph is shown in Figure 8 The most recent <br /> groundwater elevation data and inferred potentiometric surface contour lines are shown <br /> on Figure 9 Consistent with previous monitoring episodes, Aegis estimates groundwater <br /> flow is to the east at an average hydraulic gradient of approximately 0 001 ft/ft No <br /> benzene has been detected in the off-site downgradient well MW-7, indicating minimal <br /> Iplume migration <br /> 3 3 Potential Off-site Sources <br /> The groundwater samples collected from MW-3 and MW-6 contained detectable <br /> concentrations of TPHg and BTEX (Figure 10 and Table 6) Both MW-3 and MW-6 are <br /> up-gradient of the former UST basin, indicating a potential off-site source of petroleum <br /> hydrocarbons in groundwater <br /> 91-044A RAP 3 <br />