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Atlantic Richfield Company 4 <br /> ARCO 595 6100 North Highway 99,Stockton California September 13,2002 <br /> • wells MW-8 through MW-10 were installed at depths of 74 feet, 70 5 feet, and 70 5 feet <br /> bgs, respectively Shallow wells MW-8 through MW-10 were completed with 20-foot <br /> screens, extending from 53 feet to 73 feet bgs, 50 feet to 70 feet bgs, and 50 feet to 70 <br /> feet bgs, respectively Well completion details are included in Table 1 Bonng logs and <br /> well construction details are included in Attachment C Field procedures are described <br /> in Attachment D <br /> Subsurface Conditions <br /> Soil encountered during drilling activities generally consisted of interbedded layers of <br /> sands, slits, and clays A continuous clay layer is present beneath the site and site <br /> vicinity and ranges in thickness from ground surface to approximately 18 feet bgs <br /> Discontinuous sand and clay interbeds were present to the depth explored The most <br /> continuous sand interbeds were water-bearing zones encountered between the <br /> approximate depths of 60 and 70 feet and at about 98 feet deep Boring logs are <br /> presented in Attachment C Geologic cross-sections are included as Figures 3 and 4 <br /> Groundwater was first encountered in borings for shallow wells MW-8 through MW-10 <br /> and deep wells DMW-1 through DMW-3 at depths ranging from approximately 60 feet <br /> to 79 5 feet bgs Groundwater was again encountered at depths of 98 to 99 feet in the <br /> deeper borings Stabilized groundwater levels in the shallow wells ranged from <br /> • approximately 61 to 63 feet bgs during groundwater monitoring activities on July 17, <br /> 2002 (Table 2) Shallow groundwater appears to be under unconfined to semi-confined <br /> conditions within layers of sand, silty sand, and sandy silt Stabilized groundwater levels <br /> in the deeper wells ranged from 63 to 73 feet bgs This groundwater appears to be under <br /> semi-confined to confined conditions Stabilized water levels suggest some <br /> communication between the shallow and deep water-bearing zones <br /> Soil Sampling and Analysis <br /> Soil samples for logging were collected at 5-foot intervals from the borings for shallow <br /> wells MW-8, MW-9, and MW-10, from the ground surface to the total depths explored <br /> Soil samples for logging were collected at 5-foot intervals from the borings for deep <br /> wells DMW-1 through DMW-3 from approximately 49 feet bgs to the total depth <br /> explored Soils encountered during the advancement of the borings for deep wells <br /> DMW-1 through DMW-3 were not logged from ground surface to approximately 49 feet <br /> bgs, due to the close proximity of borings PSB-2, PSB-1, and the boring for well MW-7, <br /> respectively Selected soil samples were analyzed for TPHg, BTEX, and TPHd by the <br /> California Department of Health Services/Leaking Underground Fuel Tank <br /> (DHS/LUFT) method, and fuel oxygenates (MtBE, TAME, DIPE, EtBE, TBA, 1,2- <br /> DCA, and EDB) by EPA Method 8260B <br /> TPHg, BTEX, TPHd, MtBE, and other fuel oxygenates were not detected in soil <br /> samples Soil analytical results are presented in Table 3 Field and laboratory <br /> 11ARCOW5451Reportslwell tnstall3 doc <br />