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I <br />' 2003 4`' Quarter Groundwater Report <br /> SFrontier Transportation <br />' February 11, 2004 <br /> Page 3 ; <br /> First subsurface water was encountered at depths from to 1,2' bg during tank removal <br />' and monitoring well installation at this site in 1995 and 1996 Since then, shallow subsurface <br /> water has been encountered beneath the site between 6' and 10' bg Data collected in December <br /> of 2003 identified the flow of groundwater in a generally western direction beneath the site (See <br /> Figure 3, Groundwater Gradient Map) Monitoring well MW-3R was installed within the <br /> excavation backfill material, which was coarser than the native soil The permeability difference <br />' between the backfill material and native soil can cause groundwater to accumulate within the <br /> backfill material as it flows in the downgradient western direction Historic groundwater data <br /> identified a west or southwest flow beneath the site <br />' 4.0) QUARTERLY GROUNDWATER SAMPLE RESULTS <br />' On December 30, 2003, BEH contracted Del-Tech to collect groundwater samples from �,� <br /> monitoring wells MW-1 through MW-14 for laboratory analysis Groundwater parameters (pH, 1 <br /> temperature, and conductivity) were measured before, during, and after well purging (See ,dos l0):� <br />' Appendix A for Monitoring Well Field Logs) Groundwater samples were analyzed for TPH-d, 5A ;Ao <br /> TPH-g, TPH-m, BTEX, and MTBE using EPA methods 8015 modified for diesel, 8015 modified 0%�V, 'e,��Q�` <br /> for gasoline, 8015 modified for motor oil, 8020 for BTEX, and 8260 for MTBE, respectively ,� �1y9 <br /> tLaboratory analysis results for all monitoring episodes are presented in Table 1 Recent <br /> analytical reports are included as Appendix B <br /> A <br /> Historical groundwater data has identified dissolved TPH-m in monitoring well MW-3 'off v� <br /> exclusively Maximum concentrations of dissolved TPH-m were identified in MW-3 as 33,000 �o° <br /> µg/L in January 2000 using EPA method 8015 modified In January 2000, the well cover for <br /> MW-3 was destroyed allowing oily surface water to infiltrate the well BEI[ concludes that the <br /> damaged well cover caused the increase in TPH-m in MW-3 from November 1999 to May 2000 <br /> Dissolved TPH-m concentrations have remained non-detect at the site since September 2000, <br /> when the well cover was repaired BEII, therefore, has discontinued groundwater sample <br /> analysis for TPH-m at the site <br />' Laboratory analysis identified dissolved TPH-d in monitoring well MW-3 at a maximum <br /> concentration of 33,000 µg/L in January 2000 However, the groundwater results were reported <br />' as TPH-d and TPH-m combined Since then, dissolved TPH-d concentrations in MW-3 have <br /> attenuated to non-detect in April, August, and November of 2001 Groundwater analysis results <br /> from April 2002 identified dissolved TPH-d exclusively from MW-3 as 14,200 µg/L The <br /> groundwater level in MW-3 dropped to its lowest recorded depth (10 72') in April 2002 <br /> Monitoring well MW-3 was abandoned in May 2002 Replacement well MW-3R identified no <br /> detectable concentrations of dissolved TPH-d No other detectable concentrations of dissolved <br />' TPH-d were identified from laboratory analysis in any of the wells sampled since then, which <br />