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' 17 August 2004 <br /> AGE-NC Project No 01-0827 <br />' Page 5 of 6 <br />' 4.0. SUMMARY AND CONCLUSIONS <br /> Based on the data collected from the site, AGE finds <br />' • On 10 May and 10 June, ground water was encountered at a depth of approximately 23 feet <br /> btoc The ground water flow direction was inferred to be towards the east to southeast on- <br /> site, at gradients of approximately 0 01 ft/ft to 0 009 ft/ft on-site <br /> • With the exception of wells MW-5,VW-I and VW-3,all wells are"drowned"and analytical <br /> data from these wells may not be representative of the shallow ground water conditions <br /> • With the exception of benzene,the maximum concentrations of petroleum hydrocarbon and <br /> BTEX compounds were detected in the ground water sample collected from deep vapor well <br />' VW-2d on 10 May 2004, however, the highest MTBE concentration was detected in the <br /> sample collected from VW-2d on 12 July 2004 <br />' • 1,2-DCA was not detected in the ground water samples this quarter <br /> • The concentrations of benzene in sample VW-2d and MTBE in sample VW-2d were above <br /> the DHS's Primary Maximum Contaminant Levels (MCL) for drinking water However, <br />' there are no immediate plans to use the shallow and deeper ground water in the region for <br /> domestic purposes <br />' • Oxidation is a process in which a molecule or ion loses electrons Reduction is a process by <br /> which electrons are gained A measurement of the potential for these processes to occur is <br /> called ORP (Oxidation Reduction Potential) Low ORP values, detected in the source area, <br /> demonstrate the presence of generally reduced environment in the saturated zone near the <br /> source area This reduced environment is likely due to the high saline and sulfur enriched <br /> shallow water at the site Ideally, the introduction of oxygen rich air(ozone air sparging) in <br />' the source area should produce an oxidizing environment which will lead to a reduction in <br /> contaminant levels Dissolved oxygen concentrations collected from wells at the site, since <br /> operation of the ozone air sparge system commenced, indicate an adequate migration of <br />' ozone-rich sparged air into the subsurface <br /> • Generally, since the initiation of operation of the ozone-sparging system, dissolved <br />' concentrations of TPH and BTEX compounds have decreased,however, TPH-g and BTEX <br /> concentrations increased during the second quarter of sampling, suggesting continued <br /> desorption of hydrocarbons from soil into ground water <br /> 1 <br /> 1 <br />' Advanced GeoEnvironmental,Inc <br />