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CTealogctaI Tecluefes lru Page 6 <br /> Groundwater Monitoring Report <br /> Project No 425 2 <br /> January 25,2002 <br /> ' . Wells MW-4 and MW-5 contaminant concentrations exhibit a stable trend <br /> • Wells MW-102 and MW-202 did not contain contaminant concentrations above the <br /> ' laboratory reporting limits for the fifth consecutive event <br /> • All three of the domestic wells were non-detect for the event <br /> r Oxidation-Reduction Potential (ORP) was measured (Table 6 & Figure 9)- The results <br /> suggest that well MW-2 is in the core of the contamination plume or is immediately <br /> down gradient of the plume Negative ORP values indicate that the wells are within the <br /> ' halo of reaction depleted water caused by biodegradation of the contaminants For the <br /> December 3, 2001 event, seven water table wells had negative ORP values <br /> ' 3 0 CONCLUSIONS AND RECOMMENDATIONS <br /> ' The following conclusions have been drawn regarding the status of the groundwater at this <br /> site and recommendations for future work <br /> ' Conclusions <br /> 1 The water table groundwater gradient historically flowed in a northern direction at about <br /> 0 002 ft/ft prior to May 1998 However, since that time, the gradient has fluctuated <br /> from north to northeast <br /> 2 The intermediate depth groundwater has flowed easterly, with two shifts to southeast <br /> ' during September 2000 & September 2001 The direction of north for the December 3 <br /> event was anomalous and the December 21 event was consistent with the historical data <br /> 3 Vertical groundwater gradients have been found to be flowing upward during winter and <br /> ' - early spring and downward during late spring and summer This may be due to the <br /> annual cycle of groundwater pumping needs of the community The positive gradients <br /> recorded for the December 2001 events are consistent with the December 2000 event <br /> ' 4 The dominance of upward vertical flow of groundwater may be the primary reason the <br /> contaminants has not impacted the drinking water aquifer During heavy pumping, the <br /> contaminants would be moved into deeper portions of the aquifer and a slower rate then <br /> they would be moved back to a shallower depth in low pumping periods of the year <br /> 5 The shallow water table groundwater plume is laterally defined except to the west The <br /> data indicate that the contamination does attenuate toward the west <br /> 6 Petroleum hydrocarbon concentrations in the groundwater at the site fluctuate with each <br /> monitoring event The residual contamination in soil up gradient of MW-2 remains a <br /> ' significant source of impact to the groundwater plume <br /> 7 The deeper groundwater plume is defined vertically since MW-102 and MW-202 <br /> remain non-detect for contaminants <br /> 8 The three domestic wells sampled for the event remain non-detect <br /> • <br /> 1 <br />