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collect samples to confirm the vapor results The results of the investigation were presented in the <br /> Soil Assessment Report prepared by Upgradient in April 1998 Subsequently, one of the borings <br /> was converted to groundwater monitor well VM-4 <br /> In August 1999, Upgradient installed two remediation test wells within the mapped zone of soil <br /> contamination However, no hydrocarbons were detected in any of the soil samples collected from <br /> these wells One of the wells (VT-1) was screened with 4-inch PVC casing from 15 to 30 feet for <br /> future use in soil vapor extraction testing' The other well (SW-1), was screened with 2-inch PVC <br /> casing from 29 5 to 315 feet for potential use as an air sparging well <br /> (Groundwater monitoring has been performed quarterly since the middle of 1998 This report <br /> presents the result of monitoring for the fourth quarter of 2002 <br /> 4 <br /> 3.0 PROCEDURES <br /> The depth to groundwater was measured and water samples were collected on November 20, 2002 <br /> The wells were opened and allowed to equalize with atmospheric pressure before the depth to <br /> groundwater was measured Depth measurements were recorded on the Well Monitor Report <br /> (Appendix A) and are shown in Table 1 After water depths were measured, samples were collected <br /> from each well Two 40-m1 vials were collected from each, labeled, and placed in a cooled ice <br /> chest The samples were later transported to Sequoia Analytical Laboratory for analysis The <br /> laboratory report is included in Appendix B <br /> One vial from VM-2 was broken during transport, and the second vial was broken at the laboratory <br /> Therefore, a replacement sample was collected on December 27 <br /> 4.0 RESULTS <br /> 4.1 Depth to Groundwater and Hydraulic Gradient <br /> The depth to groundwater on November 20 averaged about 36 feet (Table 1), which is about 1 <br /> foot deeper than it was in September and about 3 feet deeper than at this time last year <br /> Figure 3 illustrates the hydraulic gradient and general direction of groundwater flow The <br /> contours form an arcuate pattern and slope eastward, implying that this is the predominant flow <br /> direction <br /> 4.2 Analytical Results <br /> Total Petroleum Hydrocarbon and BTEX concentrations again decreased in three of the four <br /> wells during the quarter(Table 2) In VM-1, concentrations have declined each quarter this year <br /> and are now less than 50%of their March concentrations and about 65% of their concentrations a <br /> 3 <br />