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Third Quarter 2003 Groundwater Monitoring Report <br /> Eckert Cold Storage,Manteca,California <br /> October 14,2003 <br /> Page 2 <br /> FIELD OBSERVATIONS <br /> No separate phase petroleum was noted in the wells, but a slight petroleum odor was noted in <br /> groundwater recovered from MW-8. On September 2, 2003 a Condor representative collected depth to <br /> water measurements at the site. A measurement could not be collected at MW-7, however, because plant <br /> roots were penetrating the well screened interval at approximately 20 feet below ground surface (bgs), <br /> thereby obstructing the water level probe from reaching groundwater. A Condor representative removed <br /> the root mass in MW-7 with a small-diameter auger on September 3, 2003. Field observation sheets are <br /> included in Attachment B. <br /> GROUNDWATER ELEVATIONS <br /> The average groundwater elevation was approximately 2.37 feet lower on September 2, 2003, than the <br /> previous sampling event conducted on June 5, 2003. 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 September 2, 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 that the general historical groundwater gradient is predominantly towards the northwest at the <br /> site. The highly variable gradient at the site may be related to domestic/supply well pumping both on site <br /> and off site. At times in the past, the water table slope has been very flat (very gentle groundwater <br /> gradient). When this occurs, any slight variability in groundwater measurements and the tolerance for <br /> error for the water level measurement devices can result in apparent groundwater elevation contours that <br /> are not 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 monitor wells. Consistent with this, Figure 4, Attachment A, shows the <br /> groundwater gradient direction and magnitude using monitor wells MW-4, MW-5, and MW-6. On <br /> September 2, 2003, the groundwater gradient was 0.0020 ft./ft. towards the northwest, as shown. <br /> Groundwater elevation data for September 2, 2003 are presented in Table 1, below. <br /> Table 1 --Groundwater Elevation Data (September 2, 2003) <br /> Monitoring Screened Interval(bgs) TOC Elevation Depth To Water Groundwater <br /> Well Elevation <br /> MW-1 13 -28 38.09 20.42 17.67 <br /> MW-2 15 -30 37.90 20.22 17.68 <br /> MW-3 15 -30 38.31 20.65 17.66 <br /> MW-4 12-27 37.84 20.46 17.38 <br /> MW-5 14-34 41.22 23.72 17.50 <br /> MW-6 13 -33 37.65 19.96 17.69 <br /> MW-7 13 -33 38.22 NM (Obstruction) NM <br /> MW-8 <br /> 17-37 37.76 20.27 17.49 <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 /> NM=Not Measured <br /> All measurements are in feet. <br /> A <br /> Z01� CONDOR <br />