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OW16gieal Technics&C. SOOO I%,1 Page 2 <br /> Tank Closure Testing Report <br /> Project No. 1218.2 <br /> +r August 3,2005 <br /> GeoProbe boreholes (GP-1, GP-2 & GP-3) were advanced. The locations are shown on the <br /> Site Map (Figure 2). <br /> Each of the three GeoProbe borings was advanced to a total depth of 20 feet bgs. Two (2) <br /> soil samples from each boring were selected for laboratory analysis. Soil removed from the <br /> borings and not used for laboratory analysis was used to log the geology of the subsurface. <br /> Logs were produced for each of the boreholes and these logs are attached as Appendix C. <br /> Figure 3 shows our preliminary interpretation of the approximate extent of the contamination <br /> ,r and soil types. <br /> 2.1.1 Soil Sampling Procedure <br /> �. On July 12, 2005, V&W Drilling and Geological Technics personnel mobilized to the <br /> Broadway site. Eric L. Price, GTI geologist, collected soil samples and maintained a log <br /> from the soil borings. <br /> The boreholes were advanced using a GeoProbe 5400 direct push drill rig owned and <br /> operated by V&W Drilling, a licensed drilling contractor. The GeoProbe advances a coring <br /> �. tool with a pneumatic hammer to a selected depth. Upon reaching that depth the coring tool <br /> is opened and advanced further to fill the core barrel. The soil sample enters an acetate <br /> cylinder contained in the coring tool. Upon filling, the coring tool is pulled from the hole and <br /> L" the cylinder is removed. At a chosen interval, the cylinder is cut and the selected interval is <br /> capped with Teflon foil and plastic end caps and placed on ice for shipment to the laboratory. <br /> +r The sampling technician wore disposable gloves while collecting all samples. <br /> Two soil samples from each boring were submitted for laboratory analysis and a screening <br /> L. process was used to gather information through field observations. The field screening <br /> included: <br /> • Odor (measured via OVM, a portable photo ionization detector that uses a 10.6 eV lamp <br /> +- to detect compounds with ionization potential below 10.6 eV). <br /> • Sediment type,especially grain size and clay content <br /> • Moisture content <br /> • Visible evidence of contamination (i.e., color change due to reduction of iron or <br /> discoloration from hydrocarbons and other pollutants) <br /> DetaiIs on the geology encountered during the GeoProbe survey, as well as the field <br /> observations, are included in Section 3.2, Geology and Field Observations. <br /> w.. <br /> See Appendix C, Boring Logs for more information. <br /> Lo <br />