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KEI-P89-1104 .R9 <br /> December 17 , 1992 <br /> Page 7 <br /> (designated as EB1 through EB7 on the attached Figure 1) were <br /> drilled at the site. Subsurface materials penetrated and the <br /> depths at which soil samples were collected are shown in the <br /> attached Boring Logs. <br /> The seven borings were drilled to depths of 10 to 59 feet below <br /> grade. Ground water was encountered at depths of 58 . 0 to 58 . 5 feet <br /> below grade in exploratory borings EB1 through EB4 . In exploratory <br /> borings EB5 through EB7 , which were drilled to total depths of less <br /> than 58 feet below grade, ground water was not encountered during <br /> drilling. In addition, exploratory boring EB7 was drilled at an <br /> angle of 10 degrees to the vertical . Soil samples were collected <br /> at a maximum spacing of 5 fdot intervals, at significant changes in <br /> lithology, at obvious areas of contamination, and at or within the <br /> soil/ground water interface, beginning at a depth of 5 feet below <br /> grade in each of the borings, with the exception of EB5 and EB6 , <br /> where samples were collected beginning at 4 feet below grade. In <br /> addition, only three soil samples from EB7 were submitted for <br /> laboratory analysis . The undisturbed soil samples were collected <br /> by driving a California-modified split-spoon sampler ( lined with <br /> brass liners) ahead of the drilling augers . Exploratory borings <br /> EB5 and EB6 were drilled and sampled by the use of a hand auger <br /> The clean, two-inch diameter brass liners holding the samples were <br /> then sealed with aluminum foil , plastic caps and tape, labeled, and <br /> stored in a cooled ice chest for delivery to a state-certified <br /> laboratory. Drilling was stopped about 0 . 5 to 2 feet after <br /> intersecting the first water table . Water samples were collected <br /> from borings EBI through EB4 by the use of a clean acrylic bailer <br /> The water samples were decanted into clean VOA vials and/or one- <br /> liter amber bottles, as appropriate, which were then sealed with <br /> Teflon-lined screw caps, labeled, and stored in a cooler, on ice, <br /> for delivery to a state-certified laboratory After the water <br /> samples were collected, the borings were backfilled to the surface <br /> with neat cement grout ( in accordance with the grout mixing <br /> guidelines presented in the California Well Standards , Bulletin 74- <br /> 90, dated June 1991) . Bentonite was used to seal the borings <br /> within the saturated zone. Grout was placed from the bentonite <br /> plug up to the surface in one continuous pour. <br /> ANALYTICAL RESULTS -- EXPLORATORY BORINGS <br /> All samples were analyzed at Sequoia Analytical Laboratory in <br /> Concord, California, and were accompanied by properly executed <br /> Chain of Custody documentation. Water and selected soil samples <br /> from all seven exploratory borings were analyzed for TPH as <br /> gasoline by EPA method 5030/modified 8015 , and BTX&E by EPA method <br /> 8020 . In addition, water and selected soil samples from EB3 and <br /> EB4 were analyzed for TPH as diesel by EPA method 3550/modified <br />