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First Quarter Monitoring and Sampling Report, 1993 April 14, 1993 <br /> • Southland Site No. 20304, 455 Grant Line Rd., Tracy, CA 2 <br /> casing using an QRS Environmental Equipment INTERFACE PROBE Well Monitoring System. <br /> Attachment 2 includes Groundwater Technology's Standard Operating Procedures for groundwater <br /> monitoring. <br /> Separate-phase hydrocarbons were not detected in any of the monitoring wells. The water-table <br /> elevations calculated from the March 11, 1993, monitoring data were used to prepare a <br /> potentiometric surface map (Figure 2). Wells MW-9 and MW-10 are screened into a shallow or <br /> perched water-bearing zone. Because wells MW-9 and MW-10 have repeatedly shown groundwater <br /> elevations different from those in the surrounding wells, they were not used to calculate the <br /> potentiometric groundwater surface. Data from monitoring well MW-11 indicated an anomalous <br /> groundwater elevation and therefore was not used to calculate the potentiometric groundwater <br /> surface. The potentiometric surface elevation as measured in the groundwater monitoring wells <br /> increased an average of 0.31 foot since the December 28, 1992, monitoring event. The groundwater <br /> flow direction is toward the north-northeast with a hydraulic gradient of approximately 0.003 foot per <br /> foot (ft/ft). The historical and current water-level measurements are presented in Attachment 3, <br /> Table 1. <br /> MONITORING WELL SAMPLING AND ANALYTICAL RESULTS <br /> On March 11, 1993, groundwater samples were collected from 11 monitoring wells (MW-1 through <br /> MW-6 and MW-8 through MW-12). Monitoring well MW-13 and MW-14 are sampled on an annual <br /> (January) basis because historically the analytical results have reported concentrations below the <br /> method detection limits. Before sampling, at least 4 well-casing volumes of groundwater were <br /> removed from each of the monitoring wells unless the wells were purged dry. Field measurements <br /> of temperature, conductivity, and pH were recorded during well purging (Attachment 4). The <br /> groundwater samples were collected using a Teflon® sampler and placed in analyses-specific <br /> sample containers with analyses-specific preservatives. The samples were then sealed and labeled <br /> with the job identification number, the sample number, date, time, and type of laboratory analysis <br /> required. The samples were stored on ice and transported under chain-of custody protocol to GTEL <br /> Environmental Laboratories, Inc. in Concord, California. <br /> The groundwater samples were analyzed for BTEX, TPH-G, and TPH-D by the methods noted above. <br /> The samples from monitoring wells MW-1, MW-2, and MW-4 were also analyzed for pH, nitrate, <br /> chloride, and sulfate. The sample from MW-1 was also analyzed for total lead, pesticides, <br /> polychlorinated biphenyls, and for volatile organics. Figure 3 illustrates the distribution of benzene <br /> and TPH-G. Tables 2 and 3 summarize the analytical results of this sampling event and the <br /> historical analytical data. The laboratory analytical reports and the chain-of-custody records for the <br /> March 11, 1993, samples are included in Attachment 5. <br /> R3767A1.SCH <br /> GROUNDWATER <br /> ��.._�i_�TECHNOLOGY INC. <br />