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Geological Technics Inc. Page 4 <br /> Groundwater Monitoring Report <br /> Project No.723.2 <br /> September 30,2002 <br /> As required under AB2886, the laboratory data were submitted electronically to GeoTracker <br /> on September 11, 2002 - confirmation number 6928664684. <br /> 2.0 FINDINGS AND DISCUSSION <br /> The results of the groundwater sample analysis show the following: <br /> • The concentrations of BTEX and TPH-G continue to fluctuate in individual monitoring <br /> wells from one sampling event to the next. <br /> • Intermediate well MW-101 continues to contain stable TPH-G concentrations, but <br /> benzene and toluene concentrations have fallen to non-detectable levels. <br /> 0 Deep well MW-201 continues to experience a decline in contaminant concentrations. <br /> Benzene, toluene and TPH-G concentrations have fallen to levels below the laboratory <br /> reporting limits. Ethyl Benzene and Xylene were present at 0.3 and 4.8 ug/l, <br /> respectively. MTBE was present at 2.4 gg/l but this was not confirmed by EPA method <br /> 8260. The contamination is probably a drilling artifact created by the use of mud rotary <br /> drilling. It is noted that the contaminant concentrations in MW-201 have declined by an <br /> ,r order of magnitude since the first monitoring event in December 2001, which supports <br /> the conclusion that the high concentrations were from a drilling artifact. <br /> • Figure 4 illustrates TPH-G and Benzene concentrations versus elevation in well MW-3, <br /> which lies near the core of the plume. There appears to be a direct relationship between <br /> the water table and the TPH-G concentrations. Benzene concentrations have stabilized <br /> in the well. <br /> • Figure 5 illustrates TPH-G and Benzene concentrations versus elevation in well MW-4, <br /> which lies up gradient of the core of the plume. The contaminant concentrations have <br /> stabilized in this well. <br /> 4 • Figure 6 illustrates TPH-G and Benzene concentrations versus elevation in deep well <br /> MW-101, which lies near the core of the plume. The concentrations are approaching <br /> stability. The steep decline in the initial concentrations suggests that the contaminants <br /> detected in the well were initially a drilling artifact <br /> • Figure 7 illustrates the TPH-G concentrations in the shallow wells. The high <br /> �. concentration in well MW-3 creates a localized node. Additional investigation is <br /> needed to gain a more accurate site conceptual model. <br /> 3.0 CONCLUSIONS & RECOMMENDATIONS <br /> Conclusions <br /> 1. Groundwater flow trends to the northeast to east. The southerly flow direction recorded <br /> on December 4, 2000, appears to be anomalous. <br /> 2. High levels of BTEX and TPH-G are present in the groundwater of all six water table <br /> .r monitoring wells. It is noted that the groundwater elevation exceeded the level of the <br /> w. <br />