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- -------- � u <br /> �eolaaI°I"ecFimrs Inc - -_ - - --- - - - - - - - - - - - _ - -- V —r Page S— - - --- -- µ- <br /> g <br /> Groundwater Momtonng Report <br /> Project No 425 2 <br /> February 1,2001 <br /> 3.0 CONCLUSIONS AND RECOMMENDATIONS <br /> f, 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 shifted towards <br /> 1 the northeast The cause for this shift is not known at this time <br /> 2 The intermediate depth groundwater flows more easterly then the water table, which is <br /> consistent with previous monitoring events The cause for this shift is not known at this <br /> time <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 A comparison of the <br /> December 1999 and December 2000 monitoring events reveal opposite- negative and <br /> 1 positive gradients, respectively The reason for this anomaly is not conclusive, however <br /> it could be due to fall 1999 being so dry that the community continued pumping at high <br /> rates late into the year <br /> 4 The dominance of upward vertical flow of groundwater may be the primary reason the <br /> contaminantsl&Aot 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 <br /> 6 Petroleum hydrocarbon concentrations in the groundwater at the site fluctuate with each <br /> monitoring event <br /> 7 The deeper groundwater plume is defined vertically since MW-102 and MW-202 <br /> remain non-detect for contaminants <br /> 8 Two domestic wells associated with this site remain non-detect A third intermittently <br /> contains trace toluene and xylene contamination <br /> 9 GTI has previously stated that the groundwater plume appears to pose a significant <br /> threat to public health and the environment because of the domestic wells associated <br /> with the residences surrounding the property But as wells MW-7 and MW-107 remain <br /> free of contaminants with each passing quarter, the apparent low mobility of the plume <br /> reduces the risk associated with off site groundwater receptors <br /> 1 Recommendations <br /> The following recommendations are made <br /> I The 12 monitoring wells and 3 domestic wells should be sampled for natural attenuation <br /> parameters during future monitoring events so it may be determined if remediation by <br /> natural attenuation is occurring <br />