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EM 1110-1-400'1 <br /> 3 Jun 02 <br /> b Case Study Site 2 <br /> Site 2 is located in the Central Valley of California The subsurface at Site 2 readily meets the <br /> conceptual model of mobile and immobile zones for air movement during SVE PneuLogo flow profiles <br /> revealed only about 20%of the vadose zone allowed effective air flow These mobile zones consisted of <br /> interbedded sand layers within an immobile zone predominantly made up of moist silts and fine sands <br /> Historical concentration and flow data were available from both the manifold (representing the <br /> cumulative extraction rate from all wells and the mixed contaminant concentrations), individual <br /> extraction wells, and vapor monitoring wells The history shows the concentrations rising during the <br /> first week of operation After this initial period,both the TCE and PCE concentrations exhibited the <br /> classic exponential decay The initial 90 days of extraction were performed with a single extraction well <br /> (VW-01)near the center of the suspected source area This 90-day penod was followed by additions and <br /> modifications to the extraction configuration using three other surrounding wells and two rebound <br /> periods <br /> The two-region model was applied using soil properties measured at the site and a detailed extraction <br /> history employing 193 constant flow segments over a four-year period to fit the observed PCE <br /> concentrations in the manifold and from well VW-01 The procedure followed to fit the data is outlined <br /> in Section F-5 The resulting model fits are illustrated in Figures F-5 and F-6 Similar results were <br /> achieved for TCE data The initial concentration in the mobile phase was assumed equal to the early <br /> (day 9)peak concentration observed in the manifold The other best-fit values for PCE are listed in <br /> Table F-3 The total characteristic volume of contaminated soil was estimated to be 1,099,400 cubic <br /> yards (840,600 m3)with roughly 18 % characterized as mobile and 82 %immobile For a depth to <br /> groundwater of 105 feet this yields an equivalent radius of 300 feet for the contamination This radius <br /> correlated well with the overall dimensions of observed PCE contamination at the start of remediation <br /> The characteristic diffusion length estimated for the immobile zone was about 1 15 feet(0 35 m) <br /> corresponding to an average total thickness of about 2 3 feet for each immobile zone region This <br /> characteristic length was calculated using equation(F-22)and the fit mass transfer coefficient In <br /> addition,this length is consistent with the observations from the PneuLog®flow profiles The best-fit <br /> immobile zone initial vapor concentration(565 ppmv)was equivalent to the mobile zone (650 ppmv) <br /> indicating the mobile and immobile regions were in equilibrium The values differ because differing soil <br /> properties yield differing partitioning components Using the estimated initial mobile and immobile zone <br /> PCE vapor concentrations and the best-fit total volume yielded an estimated total initial mass for PCE of <br /> 4,130 pounds (1,873 kg) <br /> F-18 <br />