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i <br /> SECTION 5 <br /> Conclusions and Recommendations <br /> 5.1 Conclusions <br /> The purpose of this investigation was to provide additional site characterization of <br /> petroleum constituents in soil and groundwater beneath and downgradient of the Disco <br /> property to reduce uncertainty regarding the migration of contaminants from the site. The <br /> investigation was successful in assessing the horizontal and vertical extent of petroleum <br /> hydrocarbons,EDB,and 1,2-DCA in soil and groundwater in the areas of concern. <br /> The CPT boring logs used in conjunction with cross-sections of the Disco property identify <br /> an apparently continuous sand unit approximately 5 to 10 feet thick,and located between <br /> approximately 90 to 110 feet below the former tank and pump area. The unit is thickest in <br /> the vicinity of MW-DIS-8S/SD and thins toward the south and east(see Figs. 4-3,4-5,4-6, <br /> j and 4-7). The unit is not present in borings CPT-9,and-13. The geometry and extent of the <br /> sand unit in conjunction with the current groundwater flow direction provide insight to the <br /> migration characteristics of the constituents of concem. A fairly continuous fine- <br /> grained/clay unit underlies the permeable zone in all CPT borings,and appears to be an <br /> effective barrier to vertical migration of compounds. <br /> Analytical results of soil and groundwater samples from this investigation indicate <br /> petroleum hydrocarbons,TBA,EDB,and 1,2-DCA are the primary constituents of concern <br /> for the Disco Site. These compounds area primarily located within the 5-to 10-foot thick <br /> sandy unit located about 90-to 100-feet below the site.The geometry,orientation,and extent <br /> of the dissolved hydrocarbon plume coincides with this permeable unit,and is consistent <br /> with the groundwater flow direction.Also,this depth coincides with the depth to <br /> groundwater in the Stockton area between 1972 and 1977(See Figure 2-2).The Disco <br /> igasoline station operated from the mid-1960's to 1976, therefore,any leaks.Qr spills that <br /> occurred during this time would have migrated downward to the top of the water table.The <br /> dissolve hydrocarbon plume appears to be confined to the sandy unit between 90 and 100 ft <br /> bgs, as supported by lithologic logs,and the shallow CPT groundwater samples. <br /> The horizontal and vertical extent of TPH-gasoline and BTEX compounds in groundwater is <br /> graphically shown on Figures 4-8 and 4-10. The horizontal and vertical extent of 1,2-DCA is <br /> shown on Figures 4-9 and 4-11. The maximum horizontal extent of TPH-gas and BTEX <br /> compounds is estimated at approximately 250 feet downgradient. The 1,2-DCA and TBA is <br /> found at least 350 feet downgradient,and the maximum horizontal extent has not been <br /> completely defined. EDB is not found in any downgradient groundwater samples. The <br /> vertical extent of the contamination is predominantly confined to the sandy zone between 90 <br /> and 110 feet below ground surface. <br /> Hydrocarbon Mass Calculation <br /> The total mass of TPH-gas present within the hydrocarbon plume at the Disco site was <br /> l estimated. TPH-gas isoconcentration plume maps in plan view,and longitudinal and lateral <br /> cross-sectional views were drafted in intervals of 200, 150, 100,50,and 20 mg/L,see Figures <br /> ti • <br /> 5FOICPT REPORT MOV003670036 rye <br />