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Geo(gicufTechnics Znc Page 6 <br /> Former Moresco Property <br /> Site Characterization Report <br /> Project No. 251.2 <br /> 16.. October 11, 1996 <br /> 3.3 Hydrocarbon Distribution in the Soil & Mass Balance <br /> Hvdrocarbon Distribution <br /> Laboratory analyses of soil samples suggest that the vertical extent of soil impacted with <br /> gasoline range petroleum hydrocarbons is presently above 70 feet bgs. The lateral extent has <br /> been defined to the south, west, east and almost to the north. The geologic cross section <br /> (Figures 3 & 4) drawn through the site from north to south illustrate the geology of the site <br /> +� and the contaminant distribution. <br /> The fuel oxygenate compound Methyl Tertiary Butyl Ether (MTBE) is present at this site and <br /> -47 may account for the apparent continued mobility of these chemicals. Because testing for <br /> MTBE did not occur until the most recent drilling and sampling event we do not have a <br /> complete understanding of the concentration or distribution of this chemical. <br /> 9"' The heart of the contamination appears to be between 25 to 35 feet below grade in a clean <br /> sand containing discontinuous silty sand lenses. Curiously, the contamination appears to <br /> have preferentially migrated toward the north as evidenced by field observations and <br /> L. laboratory data. We suspect that the upper fine grained zone between 10-20 feet may have <br /> directed contaminant flow in that direction. The concentration of contamination attenuates <br /> with depth and does not appear to have penetrated much deeper than the thin gravel layer at <br /> 63 feet. Because flow characteristics in unsaturated zones is highly dependent on the <br /> aperture of interstitial capillaries (pore space, size and permeability) we suspect that the <br /> gravel unit will temporary retard vertical movement until the overlying silty sand material <br /> becomes saturated with soil moisture/ gasoline and the capillary pressure equilibrates with <br /> L. the larger pore spaces of the gravel unit. At that time we would expect that the fine grain unit <br /> underlying the gravel will wick the contamination downward from the gravel unit. <br /> This data is summarized and shown as Tables I & 2 in Appendix A. Copies of the laboratory <br /> analytical reports are attached as Appendix C. <br /> Mass Balance Calculations <br /> Mass balance calculations were performed in an attempt to evaluate the amount of gasoline <br /> remaining in the soil. The calculations divided the impacted area into 4 layers with layers 2 <br /> through 4 having an inner and outer zone. <br /> Lo <br /> The mass balance calculations shown in Table 3 indicate that approximately 1,675 gallons of <br /> gasoline is adsorbed onto soil grains and present in a gaseous phase. The distribution of the <br /> highest mass concentration is centered around 25 feet which suggests the mass is migrating <br /> downward from the point of release at about 5 feet bgs. Relatively high levels of gasoline <br /> (-6 ppt - part per thousand) and benzene (-1 ppt) are present in the soil at 25 feet. It is this <br /> mass of chemicals that we believe may pose a threat to public health or the environment if it <br /> '- is not partially mitigated. Beneath this, detectable concentrations are present down to 60 feet. <br /> It is recommended that this information, along with the other data generated during this <br /> r.. investigation be used to evaluate the risk of leaving the chemicals in the soil and to what <br /> degree the chemicals would have to be mitigated to protect public health and the <br /> environment. This approach is discussed further below. <br /> L. <br /> Lo <br />