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A prior survey for nearby well locations, conducted by Advanced GeoEnvironmental, Inc. (AGE) in 2000, <br /> reports that none are generally located within a 1,000 foot radius, but that several exist just outside this <br /> radius(AGE, 2000). <br /> 4.0 FIELD ACTIVITIES <br /> 4.1 Direct Push Borings—Soil Sample Collection <br /> On June 10 & 11, 2004, eight soil borings were advanced to a depth of approximately 20 to 25 feet with a <br /> truck-mounted, hydraulically operated, GEOPROBE® direbt-push rig. The locations of these borings, <br /> designated B1 through B8, are shown on attached Figure 2. Detailed drawings of each specific area in <br /> which borings were advanced are also attached as Figures 3-B. <br /> Soil samples were collected in each boring at approximate five-foot depth intervals. Samples were <br /> obtained with a 24-inch long piston soil sampler lined with 1.0-inch diameter vinyl acetate tubing. Further <br /> details of the soil sample collection procedures are provided in attached Appendix A. Details of the <br /> specific soil lithology encountered in each individual boring are provided on the boring logs in attached <br /> Appendix B. All soil was logged in general accordance with the Unified Soil Classification System <br /> (USCS). <br /> 4.2 In-Situ Groundwater Sampling <br /> Upon advancing each boring into the shallow groundwater-bearing zone, a temporary well screen (.0.010- <br /> inch factory slotted) was installed into the groundwater zone to facilitate the collection of an in-situ <br /> groundwater sample. <br /> Groundwater samples were collected by installing a length of new, dedicated polypropylene tubing down <br /> the push rods to the depth of the temporary well screen. A peristaltic pump was then used to raise the <br /> groundwater to the surface, at which time it was collected in a laboratory-approved one-liter amber bottle <br /> (with I'i2SO4 preservative) and 40-milliliter glass VOA vials with TEFLON septum lids. <br /> During the sampling, observations of groundwater odor and color were also noted. This information is <br /> summarized below: <br /> - <br /> ':r i. <br /> - - - �� C:�-Y.'��.� -:IRS.r <br /> v:::::.v �,F <br /> .:... :::.:_:::,::::::::::::::::.... .:. :.,:..ter:.:..:::.::•:n•:.:r:;•::::::.:•:•.-.,,..>:.:::::;:ri rr•?::�'h•:;•: <br /> BORING NO. COMMENTS <br /> B1 Slight hydrocarbon odor in water. No discoloration. <br /> B2 Slight hydrocarbon odor in water. No discoloration. <br /> B3 Moderate hydrocarbon odor and grey discoloration in water. <br /> B4 No odor or discoloration in water. <br /> B6 No odor or discoloration in water. <br /> B6 No odor or discoloration in water. <br /> B7 Faint hydrocarbon odor and grey discoloration in water. <br /> B8 Faint hydrocarbon odor and grey discoloration in water. <br /> 4.3 Soil Litholocgv <br /> Soil types encountered during the field investigation were predominantly sand/silt mixtures, clay/silt <br /> mixtures, and occasional units fine sand. Details of the lithology encountered in each individual soil <br /> boring are provided on the boring logs in attached Appendix S. Soils were logged in general accordance <br /> with the Unified Soil Classification System (USCS). <br /> Proj. No.: 04483-01 2 of 7 AEM <br />