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E INC <br /> The local subsurface sediments in the vicinity of the Hi Hopes property have been <br /> determined by previous WZI investigations in the area (WZI, 1996b) to generally consist <br /> of a heterogeneous mix of interbedded, poorly graded to well graded sand, silty sand, <br /> sandy silt, sandy clay, and clay The silty sand and poorly graded sand generally contain <br /> fine-grained, subrounded, quartz grains with mica The well graded sands consist of <br /> subangular to subrounded quartz, feldspar, and lithic fragments <br /> 4.3 Exploratory Soil Borings <br /> Prior to submission of a final vadose zone site assessment workplan to PHSEHD, WZI <br /> prepared a site health and safety workplan This health and safety plan was incorporated <br /> as Appendix I of this report Four exploratory soil borings were drilled in the vicinity of the <br /> former Tank#1 location with the objective of identifying the overall vertical and horizontal <br /> extent of soil hydrocarbon contamination and to characterize the nature of the hydrocarbon <br /> contamination One exploratory soil boring was drilled at the former Tank #2 location to <br /> confirm all soil contamination had been removed when the tank was excavated Exhibit <br /> 5 depicts the locations of the borings and Appendix II contains logs of the individual <br /> borings Appendix III provides of description of the soil boring soil sampling protocol used <br /> to collect, label, and transport the soil samples Appendix IV presents the soil sample <br /> chain of custody and analytical laboratory results Table 2 is a summary of the analytical <br /> laboratory results of the exploratory soil borings <br /> The soil borings were drilled on August 3 and 4, 1996 by V&W Drilling utilizing an 8" <br /> hollow stem flite auger The drilling and soil sample collection was conducted under the <br /> supervision of a WZI California registered geologist The information obtained from the <br /> soil borings can be summarized as follows (1) lithology present below the former tank <br /> sites is comprised primarily of fine to coarse grained sand with minor interbedded silt and <br /> clay, (2) lithology present conforms with previously described geologic units for the Lodi <br /> area in the upper 100 feet of the subsurface, (3) the gasoline impacted soil was present <br /> 08220010 011 27 <br />