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Remedial Action Plan <br /> Frontier Transportation <br /> June 17, 2004 <br /> Page 4 <br /> 1 encountered predominantly clays with traces of interbedded sands from 0' to 25' bgs <br /> during well advancement. See Figures 3 and 4. for lithologic cross sections. <br /> ¢a First subsurface water was encountered at depths from 11 ' to bgs during tank <br /> B I removal and monitoring well installation at this site in 1995 and 1996. Since then, first <br /> subsurface water has been encountered beneath the site between 6' and 10' bgs. Data <br /> collected in March of 2004 identified the flow of groundwater in a generally western rn-{ <br /> direction beneath the site (See Figure 5, Groundwater Gradient Map). Historic first <br /> subsurface groundwater data identified a west or soutwest flow beneath the site. <br /> Groundwater was also encountered at approximately ' bgs during installation of deep <br /> monitoring wells MW- 12 through MW- 16 and MW- 18 . The potentiometric groundwater <br /> levels in these deep wells, however, were similar to the first subsurface water levels. <br /> Groundwater levels beneath the site appear to be affected by seasonal recharge. In <br /> general, the groundwater is at its yearly low in the winter and yearly high in the spring. <br /> 4.0) IMPACTED SOIL <br /> Soil sample results from the 1995 UST removal identified petroleum <br /> hydrocarbons in the northeast excavation pit where gasoline was stored. Four soil <br /> samples were collected from the pit bottom (8 . 5' bgs) and identified TPH-g between <br /> 9,800 mg/Kg to 4,700 mg/Kg and BTEX between 1 ,007 mg/Kg to 1 ,354 mg/Kg (See <br /> Appendix A for soil sample results). Laboratory analysis indicates that the gasoline <br /> USTs were the source of impacted soil in the excavation pit bottom. <br /> The site assessment performed in 1996 focused on delineation of the source, the <br /> former gasoline USTs . Borings B- 1 through B-4 and monitoring wells MW- 1 through <br /> MW-3 were advanced to various depths up to 25' bgs. Laboratory analysis identified low <br /> level concentrations of TPH-g (<34 mg/Kg) and BTEX (<1 .365 mg/Kg) in those soil <br /> samples collected from shallow depths (6' to T bgs). MTBE was identified at a <br /> maximum of 30.5 mg/Kg at 6' bgs in boring B-2 located Wof the former USTs. Soil <br /> samples collected from 9 .5' to 11 ' bgs, the approximate depth to groundwater, identified <br /> i relatively high concentrations of TPH-g, BTEX, and MTBE. Concentrations of TPH-g <br /> were observed from 1 ,300 mg/Kg to 104 mg/Kg, BTEX from 259 .2 mg/Kg to 5 .23 <br /> mg/Kg, and MTBE from 110 mg/Kg to <0. 625 mg/Kg (See Appendix A for soil sample <br /> results). Laboratory analysis indicates that most of the shallow impacted soil identified <br /> by this investigation has been removed during UST excavation. Borings B- 1 through B-4 <br /> were located 2 feet to 18 feet away from the UST removal pit and identified low level <br /> petroleum hydrocarbons from 6' to T bgs . Moreover, the elevated TPH-g, BTEX, and <br /> MTBE concentrations from the capillary fringe and saturated zone (9 . 5 ' to 11 ' bgs) <br /> indicate that petroleum hydrocarbons have migrated through the soil and impacted the <br /> shallow groundwater. The contact between impacted groundwater and soil is the source <br /> of the lateral extent of TPH-g, BTEX, and MTBE identified in soil collected from B- I , 13- <br /> 21 B-3 , 134, MW- IRA, MW- IRB, MW-2RA, MW-2, and MW-3 at 9 .5' to 11 ' bgs . <br /> ( i <br />