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Shelby Lathrop (ConocoPhill•)and Don Pratt(ARCO) <br /> 1502 N. EI Dorado Street and 16 E. Harding Way, Stockton <br /> Page 2 of 5 <br /> The EHD has redefined the zones slightly, based on soil lithology and correlation of <br /> significant sand units across the sites. The A zone includes a major sand unit from <br /> approximately 20 feet to 35 feet bgs, locally 15 feet to 35 feet bsg. The sand has <br /> variable thickness, appears to have a curving trend toward the northeast, is <br /> associated with silt laterally, and overlies a silt unit. <br /> The A zone wells on each site are as follows: <br /> 16 E. Harding Way — MW-1 through MWA 1, EW-1 through EW-7, and when <br /> DTW is less than 30 feet bgs, SVE-1 and SVE-2. <br /> 1502 N. EI Dorado Street— MWA through MW-4. <br /> The B zone as defined by SECOR includes a thin sand unit consistently present <br /> between the depths of 75 and 85 feet bgs. <br /> The B zone wells on each site are as follows: <br /> 16 E. Harding Way— DMW-1 through DMW-3. <br /> 1502 N. EI Dorado Street— MW-5 through MW-14. <br /> Between the A zone and B zone screen interval-defined hydrologic units, the EHD <br /> has identified an unmonitored hydrologic unit, herein term the B' zone, based on its <br /> lithological character. The B' zone is a silt and sand unit commonly occurring <br /> between 45 feet and nearly 75 feet bgs. Multiple layers of thick sand units are <br /> present in this unit and this zone is 'sand rich'; the sand units are. commonly <br /> separated vertically by silt intervals but locally appear to have direct contact between <br /> them. The EHD believes that the B' zone sand units are laterally and vertically <br /> extensive enough to serve as significant contaminant migration pathways. The B' <br /> interval has not been adequately monitored on either site; neither site has wells <br /> screened to monitor contaminants in this interval, although the CP site MWA <br /> appears to have just penetrated the top of a B' sand. Commonly separated vertically <br /> from the underlying B sand units by a silt interval, locally the B' sand may be in direct <br /> contact with B sand. <br /> The soil types immediately overlying and in the C zone are poorly characterized; only <br /> four samples have been collected below the B zone, all at 10-foot intervals from a <br /> single well boring. Poorly graded sand with silt was collected from 90 feet bgs, silt <br /> from 100 feet bgs, silty sand from 110 feet bgs, and poorly graded sand from 120 feet <br /> bgs. The C zone and the immediately overlying soil appear to be similar to the <br /> overlying A, B', and B zones and a significant barrier to vertical migration of <br /> contaminants is not apparent. <br /> The C zone wells on each site are as follows: <br /> 16 E. Harding Way— none. <br /> 1502 N. EI Dorado Street— MW-15 through MW-17. <br />