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�y <br /> First Quarter 2003 Groundwater Monitoring Report <br /> Eckert Cold Storage,Manteca,California <br /> April 23,2003 <br /> Page 2 <br /> • FIELD OBSERVATIONS <br /> No separate phase petroleum was noted in the wells, but a moderate petroleum odor was noted in <br /> groundwater recovered from MW-8.Field observation sheets are included in Attachment B. <br /> GROUNDWATER ELEVATIONS <br /> The average groundwater elevation was approximately 0.57 feet higher on March 28, 2003, than the <br /> previous sampling event conducted on December 9, 2002. The groundwater elevation contours (Figure 3, <br /> Attachment A) estimated from the depth to water measurements indicate the groundwater gradient was <br /> generally towards the northwest on March 28, 2003. <br /> Historical groundwater data collected by WHF, Inc. (previous consultant) indicates a highly variable <br /> gradient at the site. Review by Condor of historical groundwater gradient information provided by WHF <br /> indicates there are potential inconsistencies in the data and possibly components of the interpretation of <br /> those data, especially related to MW-5 measurements. However, Condor agrees that the general historical <br /> groundwater gradient is predominantly towards the northwest at the site. The highly variable gradient at <br /> the site may be related to domestic/supply well pumping both on site and off site. At times in the past, the <br /> water table slope has been very flat (very gentle groundwater gradient). When this occurs, any slight <br /> variability in groundwater measurements and the tolerance for error for the water level measurement <br /> devices can result in apparent groundwater elevation contours that are not particularly coherent. <br /> Therefore, when the water table at the site is relatively flat, it may be more representative to depict the <br /> groundwater gradient with a three-point construction using groundwater elevation data from three site <br /> monitor wells that circumscribe the site, allowing triangulation of the contaminant plume, including the <br /> contaminant source area. Consistent with this, Figure 4, Attachment A, shows the groundwater gradient <br /> • direction and magnitude using monitor wells MW-4, MW-6, and MW-7. On March 28, 2003 the <br /> groundwater gradient was 0.0013 ft./ft. towards the north, as shown. Groundwater elevation data for <br /> March 28,2003 are presented in Table 1, below_ <br /> Table t —Groundwater Elevation Data(March 28,2003) <br /> Monitoring Screened Interval(bgs) TOC Elevation Depth To Water Groundwater <br /> Well Elevation. <br /> MW-1 13 -28 38.09 17.86 20.23 <br /> MW-2 15-30 37.90 17.65 20.25 <br /> MW-3 15-30 38.31 18.08 20.23 <br /> MW-4 12-27 37.84 17.78 20.06 <br /> MW-5 14-34 41.22 20.98 20.24 <br /> MW-6 13-33 37.65 17.38 20.27 <br /> MW-7 1 13—33 38.22 17.95 20.27 <br /> MW-8 1 17-37___ 37.76 17.63 20.13 <br /> 'TOC Elevation: Elevations are measured from the top of the well casing and are referenced to NGS Benchmark HS4486,elevation 35.03 feet <br /> using NAVD 88 datum. <br /> All measurements are in feet. <br /> LABORATORY ANALYTICAL RESULTS <br /> The groundwater samples collected from monitor wells MW-4, MW-8, and domestic well DW-1 were <br /> analyzed for BTEX, TPH-G, and selected gasoline oxygenates/additives including MTBE by "Argon <br /> Laboratories of Ceres, California. MW-2 was not sampled as damage to the well casing during <br /> installation of the well prevents placement of bailers and pumps down the well. In a letter dated March 7, <br /> 2003, Condor proposed that the groundwater monitoring program be reduced to include quarterly <br /> sampling of MW-4, MW-8, and the domestic well; annual sampling of MW-5 and MW-7; and no further <br /> � 3 <br /> CONDOR <br />