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J. H. KLEINFELDER&ASSOCIATES <br /> 11 soil chemistry summary for the recently collected samples has been <br /> prepared (Table 2 within Appendix A). Available laboratory data (soils <br /> and ground water) including methods of analysis and detection limits are <br /> included within Appendix E. A series of soil iso—chem maps have been <br /> prepared from the available laboratory analytics and illustrate the ; <br /> occurrence and distribution of gasoline and related compounds within the <br /> vadose zone. Figures 21 through 34 show the distribution and occurrence <br /> of contaminants using contour lines of equal concentration in an areal <br /> view. Figures 35 through 38 show the distribution and occurrence of <br /> contaminants using contour lines of equal concentration in a cross—section <br /> format. Soil boring locations used in Figures 35 through 38 are shown on <br /> the Geologic Cross Section, Location Map (Figure 4). The soil iso -chem <br /> maps processed using the cross—sectional format (Figures 35 through 39) <br /> correspond in scale and location with Geologic Cross Section A—A' . <br /> i. The vertical and aerial distribution of <br /> gasoline and its associated <br /> constituents in soil are displayed on Figures 21 through 38. The <br /> L <br /> cross—sections and maps are iso—chem drawings representing the approximate <br /> i <br /> ` distri."t—ion of gasoline and associated constituents at the site. Each i <br /> soil iso—ahem drawing was generated and processed by lnteractiye Surf r r <br /> Mo lain developed by Dynamic Graphics using a Digital Equipment <br /> Corporation VAK-11/750 computer. The computes printouts were then hand i <br /> f <br /> adjusted to fit the gaologic conditions and data boundaries not included <br /> t E <br /> in thr•. computer program. These drawings (Figures 21 through 38) were <br /> i <br /> constructed using probable geologic pathways, geologic controls and data <br /> boundaries. <br /> The following scenario preser..s a probable series of events describing the <br /> migration of contamination through the soil from two point sources. The <br /> r s direction for migration of the contamination at the site is based <br /> gravity controlled pathways derived from an interpretation of the <br /> geological conditions observed at the site. The following scenario is <br /> ` only one of many interpretations that could be made from the data so far <br /> accumulated. This interpretation does not take into consideration <br /> contamination from sources cutside of the boundaries of this site. <br /> ` 53-87-443 20 <br />