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1 <br /> Corrective Action Plan <br /> MW-7-P at a depth of 20 feet bgs. No hydrocarbons above the laboratory reporting limits were <br /> ' detected in any of the other five samples analyzed(see Table 1). The water table elevation at the <br /> time these wells were installed was approximately 17 feet bgs. Both wells were completed at a <br /> depth of 30 feet bgs. The wells were screened in the interval from approximately 8 feet bgs to <br /> t the bottom. The size for both wells are 4-inch-diameter casing installed in a 12-inch-borehole. <br /> Well construction details are presented in Table 2. Wells MW-7-P and MW-8-P are generally <br /> upgradient from the source of the contamination. <br /> ' On May 16, 1997, groundwater elevation measurements and sampling were conducted at the site <br /> by OST. Due to site access restrictions, the off-site monitoring wells, MW-7-P and MW-8-P, <br /> ' were sampled by Park on May 30, 1997. The groundwater analytical results of the most recent <br /> monitoring are presented in Table 3 and on Figure 3. The groundwater elevations are presented <br /> in Table 4, and the elevations and gradient are plotted on Figure 4. To provide a summary of the <br /> results of all previous groundwater monitoring events, a copy of Park's April 1996 Groundwater <br /> Monitoring Report is included in Appendix C. Certified Analytical Reports and field data sheets <br /> are included in Appendix D. <br /> ' 3.1 Impacted Soil <br /> ' Based upon careful review and consideration of the results of soils analyses derived from the <br /> previous investigations cited above, OST estimates the radius of impacted soil in the vadose zone <br /> M to be less than 15 feet surrounding the former UST. The average hydrocarbon concentration in <br /> this zone is estimated to range between 2,500 mg/kg and 5,000 mg/kg. The soil in the <br /> intermittently saturated"smear zone" (vertical interval of water table fluctuation) is estimated to <br /> ' have been impacted to some extent over an area roughly approximating the impacted groundwater <br /> plume. This zone is approximately 10 feet thick ranging from around 15 feet bgs to <br /> approximately 25 feet bgs. The average hydrocarbon concentration in this zone is estimated to <br /> be within 100 mg/kg to 200 mg/kg. Based upon the highest concentrations detected in the soil w <br /> at the site,with various assumptions as to their lateral and vertical extent, OST estimates as little Al� <br /> as 3,500 pounds (lbs) of petroleum hydrocarbons to as much as 8,500 lbs to be present. The <br /> ' most likely total estimated amount is 4,500 lbs. <br /> 3.2 Impacted Groundwater Plume <br /> ' The plume of impacted groundwater is estimated from the reported record of all previous site <br /> ' investigation and groundwater monitoring events. The plume is estimated to cover an area <br /> approximately 190 feet long by 90 feet wide and oriented to the northwest as illustrated on Figure <br /> 5. Although the illustrated interpretation is not the only one reasonable from the cited data, <br /> ' alternative possible interpretations would not alter the proposed plan to remediate the soil and <br /> groundwater at the site. The highest concentrations of impacted groundwater have been found <br /> in monitoring well BEI-MW3, presumed to be located at the source. In fact, the most recent <br /> monitoring event by OST reported TPHg and benzene concentrations in BEI-MW3 at their <br /> highest level ever at 110,000 micrograms per liter(µg/l) and 11,000 µg11, respectively. The next <br /> ' OST <br /> 701-1-2.cap <br /> Page 6 <br />