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p <br /> ��ME <br /> . <br /> PRO13LEM ASSESSMENT REPORT <br /> Moore Petrofeun, Inc. <br /> 1399 E. Yosemite Avenue, Manteca, to <br /> NGA Project No. 10.90-480 <br /> Page 5 <br /> well screen were backfilled with approximately two feet of clean <br /> soil overlain by plastic sheeting covering the base of the tank <br /> basin. The sections of well screen were manifolded together and <br /> brought to 2 feet below grade with sections of 4-inch-diameter PVC <br /> blank casing. Following manifolding of the PVC ;well screen, the <br /> tank basin was backfilled with clean soil. After compaction of <br /> sails used to backfill the tank basin, the tank basin was <br /> resurfaced with asphalt. A plan view of the below-ground <br /> components of the soil venting system is presented as Figure 3. <br /> 3.4 site soils and Goo2-ogy <br /> The surface of the site consists of a two--inch-layer of asphalt <br /> which overlies a four-inch-thick aggregate base. Subsurface <br /> geology at the site has been inferred from soil borings drilled by <br /> ETS, Delta, and NGA. Examination of soil borings logs indicate <br /> that soils underlying the site consist predominantly of strata of <br /> silty sand, sand, clayey sand, and silty clay. The uppermost <br /> strata encountered by soil borings is a sand which is in places <br /> both silty and gravelly. This layer ranges from about 14.5 to 20 <br /> feet thick. Thin clay lenses (less than six inches thick) were <br /> found at the base of this strata in wells MW--2 and MW-3. <br /> Underlying the uppermost sand are layers of silty sand and clayey <br /> sandand silty clay. These strata appear to grade laterally into <br /> layers of salt and silty send between MW-2 and MW-1A. A silty sand <br /> is the deepest unit penetrated at the locations of MW-2 and MW--3. <br /> Split spoon samples were not retrieved from the base of NW-1A, <br /> however, drill cuttings indicate that the deepest unit penetrated <br /> within KW-1A may be a strata of clay and gravel. Subsurface <br /> geology at the site can be more easily interpreted by examination <br /> � r of the geologic cross--sections presented in Figures 4. Cross- <br /> section locations are shown on Figure 2. <br /> .4.5 Soil Analytical Results <br /> soil samples collected from soil borings drilled by ETS, Delta, and <br /> NGA have been submitted to a California-certified laboratory and <br /> analyzed for those parameters listed in Section 1.2. Analytical <br /> results indicate that TPH have been found in samples from soil <br /> borings SB-1, SB-2, SB-3, and MW-2 at either nor,-detectible or very <br /> low concentrations. ;,oncentrations of BTEX constituents in soil <br /> samples from these borings have either been non-detectible or <br /> detected at concentrations not exceeding 0.07 part per million <br /> (Ppm) . <br /> Soil samples collected from MW-1 and KW-3 have also shown very low <br /> concentrations of BTEX. BTEX concentrations in soil -samples from <br /> _...---------these borings--do..-spot-.exceed--1.-0...-..ppm•---..-_TPH_.-conc.entr.ations. of -- <br />