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4491 Durham Ferry Road Page 3 <br /> The summary of shallow groundwater contamination failed to include the results of <br /> the grab groundwater samples which were collected from hydropunches, HP1 - <br /> HP6 drilled on October 20, 1993. The report estimated that the radius of the <br /> groundwater plume was 50 feet. It is difficult to conceptualize this estimate when <br /> the radius of the soil vadose zone contamination plume was estimated at 70 feet. <br /> The groundwater contamination plume is at least as large as the soil contamination <br /> plume. <br /> Feasibility Study <br /> A series of feasibility tests were conducted between December 19 and December <br /> 21 , 1995 to evaluate groundwater extraction, soil vapor extraction and air sparging <br /> remedial alternatives. <br /> Contaminated groundwater water was produced by the pumping of RW1 which <br /> reportedly was stored on site in a 21,000 gallon tank pending removal by a <br /> licensed hauler. Please submit documentation for the disposal of this water. A <br /> l"groundwater sample was collected on December 20, 1995 from RW1 following the <br /> completion of the test and reported on Table 2. Unfortunately, there also was an <br /> terror in the reporting of these results on Table 2 that requires revision and re- <br /> submittal. The concentration of toluene that was detected was 2.3 ppb rather than <br /> 2 ppb. <br /> The text of the report indicated that Figure 10 illustrated the water table elevation <br /> at the end of the groundwater extraction test when in fact Figure 10 described the <br /> pre- and post-sparge test results of dissolved oxygen. <br /> The report included the conclusion that it would only be possible to achieve a 35 <br /> foot soil vapor extraction radius of influence in RW1 by concurrent groundwater <br /> extraction to lower the water table. The report also stated that the radius of <br /> influence for VW2 and VW3, without groundwater extraction, was 20 and 17 feet <br /> respectively. Radius of influence data was not collected for VW1 which had <br /> vacuum versus flowrate characteristics more similar to RW1 than VW2 and VW3. <br /> Groundwater extraction may improve the radius of influence that may be acheived; <br /> however, the added costs may not justify its application over additional soil vapor <br /> extraction wells. <br /> Air sparge well, SP2 was reportedly used for air sparge testing. Air pressures of <br /> up to 15 psi were used and stabilization achieved at 7 psi with a 13 cfm flow rate, <br /> followed by a further reduction to 3 psi with a 10 cfm flow rate, in attempts to <br /> capture sparge vapors using VW3 which is approximately 45 feet away. The <br /> results were reportedly depicted on Figure 11 when actually it is Figure 10. <br /> PHS/EHD questions the results since the concentrations of dissolved oxygen <br /> observed in SP2 showed little influence by sparging. The largest change in <br /> dissolved oxygen concentrations were actually observed in SW 1 . <br />