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�' ic..sty �.1 .- <br /> a�. <br /> { <br /> 1 <br /> 13 ,July 1992 <br /> (GeoAudit CV 55-59 E2-1.32) <br /> Page 3 of 8 <br /> Samples arere transmitted to WEST laboratories for analysis. All <br /> samples were analyzed for the presence of heating oil in accordance <br /> with EPA method 8015 modified for diesel. Selected samples were <br /> also analyzed for the presence of volatile hydrocarbons (BTEX <br /> compounds) in accordance with method 8o20. The required detection <br /> limits for TPH were obtained, but high levels of motor oil and a <br /> diesel contamination interfered With the detection of BTE&X � <br /> compounds, raising the detection limit from the require 50.005 <br /> mg/kg to I mg/kg in SB-1 and SB-2 and to 0.05 mg/kg <br /> he <br /> chain-of-custody documents are attached to this report. <br /> 3.3 SUBSURFACE STRATIGRAPHY <br /> Figures 3 and 4 illustrate the shallow stratigraphy at the site. <br /> tions ishown in Fiure 2- All <br /> The location of these cross sec <br /> senetrated very similar <br /> borings are relatively close together and p <br /> materials. From the surface to a depth of e-10feet, <br /> most boorted <br /> penetrated medium yellow-brown to dark-brown, generally <br /> fine-grained to very fine-grained top eofSa��f' A thin grave ew borings, an 1-sand-clay <br /> lens was present near the top <br /> representsnbackfill <br /> retmaterial. <br /> inma clay few samples. <br /> orclay clasts were also <br /> observedauger <br /> Boring SB-4 and borings SB-6 through SB-8 penetrated a thin bed of <br /> brown silt from about 10 to 12 feet. This bed is present at <br /> SB- milar bed is <br /> approximately the same depth in SB-1 and bad was not g and a sreco nized in <br /> present in SB-5 at about 5-7 feet. This a.i <br /> SB­3, but this may be due to the fact that only a 5-inch sampTeniy <br /> _ obtained because of sampling problrms. The silt bed is app <br /> somewhat consolidated, causing drilling rates to decrease through <br /> this interval. <br /> From about 12 to 18 feet, all borings penetrated medium to light- <br /> brawn or light yellow-bro <br /> wn fine to medium-grained sand. This bed <br /> was locally oxidized to reddish-brown. Coarse-grained, gray, <br /> unweathered granitic sand is present at a depth of approximately 18 <br /> feet. This sand is very well sorted and much coarser grained than <br /> the overlying units. <br /> Barings 58-2, SB-3, SB-5, and SB--7 recovered light yellow-brown <br /> silt at a depth of 25 feet; the deepest boring, SB_7, was_st .11_ n <br /> this bed at the total depth of 30 feet. <br />