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M&MAutomotrve <br /> August 31 2000 <br /> • <br /> Reconnaissance Groundwater Sampling <br /> Groundwater from each borehole was sampled using a GeoProbe designed discrete water- <br /> sampling device in the uppermost aquifer Depth to groundwater measurements were <br /> made to the nearest one-one hundredth of one foot from existing grade, and also checked <br /> for the presence of separate phase product The groundwater sample was carefully <br /> collected with a clean disposable bailer and poured into the appropriate laboratory <br /> prepared container with minimum cavitations and headspace Each water sample was <br /> labeled, logged onto a chain-of-custody form, and placed in a chilled ace chest on crushed <br /> ice for transport to the laboratory <br /> Subsurface Conditions <br /> One exploratory boring was drilled at the location shown on Figures 1, and was advanced <br /> to a termination depth of 32 feet The boring initially revealed a pea gravel backfill from <br /> the excavation activity This backfill extended to about 10feet <br /> Silty clay underlies the backfill to a depth of 14 feet, which was stained gray and <br /> displayed petroleum vapor and odor These strata are underlain by a clayey sand to sand <br /> to a depth of about 21 feet The staining and vapors decreased with depth, with none <br /> observed by 19 feet A sample was lost at 19 to 21 feet, but sand and salty sand strata <br /> underlie the clayey sand Thin clay interbeds occurred in the silty sand at depths of 31 to <br /> 3 2 feet <br /> Groundwater occurred at depths of about 15 feet and rose in the encased boreholes to a <br /> depth of 9 35 feet, suggesting the aquifer strata may be unconfined to weakly confined <br /> Historic groundwater data shows flow to the north <br /> Regional lithologic lateral and vertical variation are present in the shallow aquifer strata, <br /> which are typical for raver and floodplain deposits in this portion of the San Joaquin <br /> Valley (see Geologic Cross Section, Figure 3) While lateral and vertical variation are <br /> present in the aquifer strata, these strata as a whole form the uppermost water bearing <br /> aquifer (or hydro-) stratigraphy between about 10 to 30 feet in the area explored <br /> Chemical Analysis <br /> Five soil samples, and two groundwater samples were analyzed at a Chromalab, Inc State <br /> certified analytical Iaboratory from the exploratory borings These samples were tested <br /> for the following, Total Petroleum Hydrocarbons as Gasoline (TPHG), Benzene (B), <br /> Page 3 <br /> St7lmso/cust/m&m <br />