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3.0 CONCLUSIONS, RECOMMENDATIONS AND PROJECT STATUS <br /> Between June 29, and September 21, 2005, the groundwater surface dropped an average of 1 09 <br /> feet, the groundwater gradient increased from 0 0104 to 0 0114 foot/foot, and the groundwater <br /> flow direction remained toward the northeast These groundwater surface characteristics are <br /> consistent with historical and seasonal trends <br /> Between June 29, and September 21, 2005, gasoline compounds in groundwater generally <br /> decreased at MW-1, and remained relatively consistent at MW-2 and MW-3 Concentrations of <br /> gasoline compounds in groundwater at MW-1 have generally declined, since the monitoring wells <br /> were installed in July 2002, probably due to source removal efforts and natural attenuation <br /> processes Since March 2004, concentrations of MTBE have been detected in the perimeter <br /> wells (MW-2 and MW-3) During the third quarter of 2005, the MTBE concentrations detected in <br /> MW-2 and MW-3 were both below the state of California Secondary Maximum Contaminant Level <br /> (MCL) of 5 µg11 <br />' On November 1, 2005, EHD met with representatives of the San Joaquin County Facilities <br /> Management Department In a letter summarizing the meeting dated November 17, 2005, EHD <br />�• states that <br /> There is a sand lens at 35 feet bgs at this site that may be a migratory pathway for the <br />' MTBE contamination It was discussed that placement of soil borings up-gradient <br /> (southwest) and cross-gradient(southeast) of MW-9 and obtaining soil samples and grab <br /> water samples from 35 feet bgs may provide definition for the site If those samples are <br /> non detect then the site should be evaluated to see If further investigation is needed <br />' Ramage Environmental recommends that a work plan be prepared that outlines the scope of work <br /> requested by EHD in addition, the plume of impacted groundwater should continue to be <br />' monitored on a quarterly basis to further evaluate natural attenuation of the plume of impacted <br /> groundwater <br /> r <br /> I <br /> I <br /> I <br /> 7 <br />