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4 KLEINFELDER <br /> ' P5 were advanced adjacent to the dry wlls located at the base of the stands ell located in the interior Race Track Area. <br /> nd <br /> pushprobe P3 was advanced near the dry <br /> The five push probes in the Dry Wells Areas were advanced to approximate total <br /> depths that ranged between 26 and 33 feet below ground surface (bgs). The AST <br /> pushprobe was advanced to approximately 16 feet bgs . Groundwater was not noted <br /> in any of the pushprobe borings. According to Kleinfelder's ESA findings, the local <br /> flood control district shows depth to groundwater in the Spring of 1999 near the site at <br /> approximately 45 feet bgs. According to depth to water data from Gillies Trucking <br /> located approximately 1700 feet to the east depth to groundwater is approximately 65 <br /> feet as of the fourth quarter of 2004. <br /> ' The push probe borings were pneumatically advanced using a 4 foot steel core barrel. <br /> Soil samples were continuously collected by inserting a new four foot acetate liner into <br /> the probe prior to each drive. Soil samples obtained for potential chemical analyses <br /> were collected at desired intervals by removing the acetate liner o and cutting out the <br /> desired 6-inch interval. The soil samples were sealed with Teflon film and plastic end <br /> caps. Two soil samples were collected from each pushprobe boring at depths ranging <br /> from 6 to 32 feet bgs (See sample collection depths in boring logs in Appendix A). <br /> Samples submitted for analysis were also collected at depths ranging from 6 to 32 feet <br /> ' bgs. Both soil samples in the AST Area at depths of 6 and 15 feet bgs were analyzed <br /> and at least one and up to two soil samples from the dry well borings were analyzed. <br /> Most of the soil samples submitted for analyses in the dry well areas were collected <br /> near the total depth of the respective borings to evaluate potential contaminants <br /> leaching from the base of the dry wells into the adjacent vadose zone. <br /> During the advancement of the push probes, Kleinfelder collected soil samples for logging <br /> 1 purposes, field screening and potential chemical analysis. No unusual odors or soil <br /> discoloration was noted in the continuous soil cores generated during advancement of the <br /> pushprobes. <br /> Soils were noted as interlayered silty sand (fine grained), clayey silt, and silty clays. Silts <br /> ' and fine sands were predominant. For additional details see boring logs in Appendix A. <br /> 4.2. INTERIOR RACE TRACK AREA <br /> A total of 14 soil samples were collected from six hand-auger borings which were <br /> advanced to a maximum depth of approximately 5 feet bgs on July 7, 2005. The six <br /> locations were located within the interior track area on grass and dirt areas. Two <br /> locations (HA2 and HA3) were located near the two turns in the track and one near a <br /> drive entrance (HA1) to the central portion of the track (as divided by a K-rail). The <br /> three remaining locations (HA4, HA5 and HA6) were located near the central portion of <br /> the track. Plate 2 illustrates the approximate location of the six hand auger borings. <br /> The soil samples were collected at depths ranging from 1 to 5 feet bgs. Eight of the 14 <br /> soil samples collected at depths ranging from 3 to 5 feet bgs were submitted for <br /> Page 10 of 22 <br /> 58671.E02/ST05R1127/DH:ly September 15, 2005 <br /> ©2005 Kleinfelder, Inc. <br />