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r ! <br /> November'l2, 1996 <br /> Page 10 <br /> i <br /> Lower we16 —MOlecular components of gasoline volatilize more ` - <br /> '� readily than the higher molecular weight components As a result the <br /> g g p , <br /> volatilization rate of TPPH-g decreases with time even though hydro- <br /> carbon-impacted soils remain within the radius of influence of the SVE <br /> wells <br /> i <br /> Clays, silts, and organic carbon, components of soils found beneath the <br /> site, tend to hold hydrocarbon impact in place This phenomenon <br /> limits the fraction of soil bound hydrocarbons that may be removed by <br /> physical means <br /> Remaining Petroleum Hydrocarbon Impact <br /> Available data (groundwater monitoring and site analytical data) indicate that the <br /> primary sources of petroleum hydrocarbons were the former gasoline USTs <br /> (northeastern portion), and the southern end of the product island located northeast of <br /> the former gasoline USTs (Figure 2) These site improvements were removed in 1988, <br /> consequently, all primary sources have been removed from the site <br /> The secondary sources of petroleum hydrocarbon residuals include (1) soils impacted <br /> with petroleum hydrocarbons, and (2) groundwater containing dissolved petroleum _ <br /> hydrocarbons The current concentration and physical extent of these residual concen- <br /> trations have been defined and significantly reduced by the application of approximately - <br /> 2 years of SVE which has been performed at the site The operation of the former SVE <br /> system was terminated when the petroleum hydrocarbon concentration in the influent <br /> stream reached an asymptotic condition <br /> 1 4 � <br /> The concentration of the residual hydrocarbons in soils are characterized by the presence <br /> of the relatively high molecular weight compounds TPPH-g concentrations range in <br /> concentration from less than 10 to 10,000 ppm Benzene with few exceptions has not <br /> been detected <br /> Residual hydrocarbons as dissolved hydrocarbons are primarily affected by <br /> (1) hydrocarbon-affected vadose-zone soils typical r-of source areas, (2) residual hydro- <br /> carbons left in soil by groundwater fluctuation, (3) operation of the SVE system, and <br /> (4) intrinsic remediation (mechanisms including biodegradation, chemical oxidation, and <br /> adsorption/absorption) Dissolved hydrocarbon concentrations in groundwater samples <br /> collected from Wells MW-4 and MW-9, located in the source area, have generally <br /> decreased with the overall increase in groundwater elevation This trend indicates that <br /> SVE was effective in remediating hydrocarbon-affected soils in the source area <br /> Dissolved hydrocarbons were not detected in groundwater samples collected from ` <br /> 4 <br /> 3201337BiCLOSLTRE2 <br /> I <br /> I ' <br /> 4 <br /> f <br />