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plume approximately 400 feet long by 250 feet wide. Once the source is removed (which is <br /> the objective of AS/SVE), all that remains is dissolved-phase groundwater contamination. <br /> Fate and Transport <br /> The current fate of smear zone NAPL is stripping by AS/SVE and biodegradation through <br /> enhanced aeration of groundwater and soil vapor. In brief, the current fate mechanisms <br /> affecting dissolved-phase gasoline are hydrodynamic dispersion; dilution, adsorption, <br /> volatilization, and biodegradation through aerobic and anoxic processes. Groundwater <br /> movement is estimated to be at a rate of 5 to 10 feet per year horizontally and 1.0 foot per <br /> year, or less, vertically. An estimated 3 percent organic fraction in the A Zone will contribute. <br /> to retardation of contaminant migration. <br /> The estimated 160 pounds total mass of dissolved phase gasoline in the plume is based on the <br /> following assumptions. <br /> { + Soil porosity is 25 percent. <br /> + The contaminated groundwater zone is a triangularly shaped block 400 feet <br /> long by 250 feet wide by 60 feet deep. <br /> + The average concentration in the plume is 3.3 mg/L TPH(g) or '/, of the <br /> 10 mg/L TPH(g)concentration measured in MW-DIS-2. <br /> If the first order rate coefficient for biodegradation of BTEX constituents is assumed to be eo' <br /> between -0.01 and -0.001 per day, the initial. rate of BTEX removal by biodegradation is <br /> between 1.4 and 0.14 pounds per day. The removal rate is expected to decline asymptotically <br /> with concentration. <br /> Exposure Path Analysts <br /> The nearest groundwater receptors are deep water supply wells located more than 3,000 feet <br /> from the Disco site. Closed wells within a 3,000-foot radius include three Del Monte <br /> production wells and two California Water Company wells that are all screened below 250 <br /> feet or so, significantly deeper than the naturally confining A and --LB- onn the <br /> gasoline plume from the Disco site. Inexpensive domestic drinking water supplied by <br /> California Water Company and excessive depth to the water bearing formation drastically <br /> limit the potential.for new private water-supply wells. It is very unlikely that gasoline <br /> constituents from the Disco site could ever reach a drinking water source or a surface water <br /> course, unless a new well is constructed with a screen interval in the shallow A or B Zone. <br /> Soil contamination above the groundwater is limited to the area directly below the footprint <br /> of the former service station, as indicated by soil borings documented in the RDFS. NAPL <br /> gasoline staining of auger cuttings was first encountered at a depth of 30 feet directly below <br /> the former tanks and piping. Therefore, contact with contaminated soil is not likely unless a,_ <br /> deep excavation is,made in the immediate vicinity o f the former tanks No such activity is f <br /> planned or anticipated.­­... <br /> SF010030983.DOC 4-2 <br />