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Rodger Liston <br /> Darpetro Inc. <br /> 749 E. Charter Way, Stockton, California <br /> Page 2 o15 <br /> summary description of contaminant sources , masses or distribution in soil <br /> included in this or any other portion of the SCM . The SCM included two cross <br /> sections , but had no reference map showing the lines of cross section or boring <br /> locations. <br /> The SCM section titled 'Groundwater Concepts' refers to hydraulic conductivity <br /> determinations obtained by slug tests on monitoring wells MW-4 , MW-5 and <br /> MW-6 , which yielded an average conductivity of 2. 94 feet/day as determined by <br /> Bouwer-Rice method . This may be an overestimate of the hydraulic conductivity <br /> as the test was conducted by adding water to the well when the water table <br /> occurred within the screen interval (Driscoll , 1986) . If this is so , then the average <br /> seepage velocity estimate of 0 .07203 feet/day would also be an overestimate . <br /> The SCM notes that a water sample could not be collected at 45 feet below <br /> surface grade (bsg) in HP-2 , but was later collected at 55 feet bsg at the same <br /> location , and inferred that the lithology at 45 feet bsg could not transmit water, <br /> forcing the ground water to migrate around and under the tight soil . The SCM <br /> also noted that dissolved methyl tert-butyl ether (MTBE ) concentrations <br /> increased from undetectable concentrations at 39 feet bsg to 2 . 1 micrograms per <br /> liter ( µg/I) at 50 feet bsg and to 16 . 5 µg/I at 60 feet bsg in boring 13-3 . CGG <br /> interprets these data as indicating northeastward flow of impacted ground water <br /> at 55 feet bsg and implied that the known UST releases to the west were <br /> potentially the sources of the contaminants . <br /> Concerning the interpretation of the HP-2 and B-3 data , EHD notes that several <br /> factors can influence the success of obtaining grab groundwater samples and <br /> that a number of factors can also influence contaminant distribution , i . e . , soil <br /> composition , vadose vs. saturated zone , proximity of source, etc. While an <br /> adequate site conceptual model may demonstrate CGG's interpretation to be <br /> correct, EHD finds the current SCM to be less than compelling . <br /> As discussed during meetings with you and your consultant on 19 June 2002 and <br /> on 07 May 2003 , to demonstrate that a plume is impacting your site from another <br /> site , a site conceptual model should be prepared that incorporates lithological <br /> and analytical data from your site and the adjacent or nearby sites, especially <br /> those suspected of being a source of contamination impacting the site . At the 07 <br /> May 2003 meeting , you and your consultant agreed to review EHD files for the <br /> data from the adjacent or nearby sites . The SCM as submitted contains no data <br /> from adjacent or nearby sites . As submitted , the SCM is not adequate to <br /> demonstrate migration of a plume onto your site, plume stability or contraction , <br /> delineation of the adsorbed and dissolved contaminant masses or vertical extent <br /> of impacted ground water. The components and purposes of an SCM were <br /> discussed with you and CGG at both meetings . Simply stated , the purposes for <br /> such a model are to demonstrate where the contaminants came from , where they <br />