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VV so' <br /> Second Quarter 2004 Groundwater Monitoring Report <br /> Eckert Cold Storage,Manteca,California <br /> July 26,2004 <br /> Page 2 <br /> FIELD OBSERVATIONS <br /> 10 On June 23, 2004, a Condor representative made field observations at two of the eight site monitoring <br /> wells (MW-4 and MW-8), and the site domestic well (DW-1). Field observations included sample odor, <br /> appearance (color, clarity, and presence of petroleum product sheen or phase in samples), and water <br /> quality field parameters. No petroleum sheen or product phase was noted in the field inspection samples <br /> collected from monitor wells MW-4 and MW-8. A moderate petroleum odor was noted in the inspection <br /> samples collected from monitor wells MW-4 and MW-8. <br /> GROUNDWATER ELEVATIONS <br /> All eight of the site monitoring wells were measured for water level during this quarterly monitoring <br /> event. The average groundwater elevation was approximately 2.01 feet lower on June 23, 2004, than the <br /> previous sampling event conducted on March 17, 2004. <br /> Historic groundwater data collected by WHF, Inc. (previous consultant) indicates a highly variable <br /> gradient at the site. Review by Condor of historic groundwater gradient information provided by WHF <br /> indicates that the general historic groundwater gradient is predominantly towards the northwest at the site. <br /> The highly variable gradient at the site may be related to domestic/supply well pumping both on site and <br /> off site. At times in the past, the water table slope has been very flat (very gentle groundwater gradient). <br /> When this occurs, any slight variability in groundwater measurements and the tolerance for error for the <br /> water level measurement devices can result in apparent groundwater elevation contours that are not <br /> particularly coherent. Therefore, when the water table at the site is relatively flat, it may be more <br /> representative to depict the groundwater gradient with a three-point construction using groundwater <br /> elevation data from three site monitoring wells. Consistent with this, the three-point solution using <br /> monitoring wells MW-3, MW-4, and MW-6 is shown in Figure 3, Attachment A. On June 23, 2004, the <br /> groundwater gradient was approximately 0.002 ft./ft. towards the northwest, consistent with historic <br /> groundwater gradient estimations. Groundwater elevation data for the June 23, 2004 monitoring event are <br /> presented in Table 1,below. <br /> Table 1 —Groundwater Elevation Data (.lune 23, 2004) <br /> Monitoring Screened Interval (bgs) TOC Elevation Depth To Water Groundwater <br /> Well Elevation <br /> MW-1 13 -28 38.09 21.49 16.60 <br /> MW-2 15 -30 37.90 21.27 16.63 <br /> MW-3 15 —30 38.31 21.70 16.61 <br /> MW-4 12-27 37.84 21.44 16.40 <br /> MW-5 14-34 41.22 24.69* 16.53* <br /> MW-6 13-33 37.65 21.05 16.60 <br /> —i MW-7 13 -33 38.22 1 21.56 16.66 <br /> MW-8 17-37 37.76 21.24 16.52 <br /> 'TOC Elevation:Elevations are measured from the top of the well casing and are referenced to NGS Benchmark HS4486,elevation 35.03 <br /> Feet using NAV D 88 datum. <br /> All measurements are in feet. <br /> * Eckert indicated that they repaired MW-5 prior to the first quarter 2004 rnonitoring-vent,with no apparent change iii cicvaliun Lu the well <br /> measuring point. <br /> r <br /> i/� CONDOR <br />