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i <br /> CGealrgical Technics Inc. Page 5 <br /> Groundwater Monitoring Report <br /> Project No. 1030.2 <br /> May 7,2003 <br /> Parameter Source of the Background Plume Plume <br /> ' Parameter Behavior Behavior <br /> Core Margins <br /> Nitrate' e"Acceptor Slightly Enriched Depleted Not Depleted <br /> Ferrous Ironz Metabolic Byproduct Slightly Enriched Slightly Enriched Not Enriched <br /> Sulfate' e"Acceptor Site Specific Slightly Enriched Mildly Depleted <br /> Temperature Metabolic Byproduct Site Specific Elevated Slight Elevated <br /> ' pH Metabolic Byproduct Site Specific Slightly Lower Slightly Higher <br /> Alkalinity Metabolic Byproduct Site Specific Enriched Mildly Depleted <br /> Redox Potential Metabolic Byproduct Negative Value Depleted Slightly Lower <br /> Conductivity Metabolic Byproduct Site Specific Elevated Unaffected <br /> e =electron <br /> Terminal electron accepting process: <br /> 1 —denitrification <br /> 2=reduction <br /> The test results showed the following: <br /> • MW-1 has a high level of alkalinity compared to MW-2 and MW-3. Elevated levels of <br /> alkalinity are an indicator of benzene biodegradation, either aerobic or anaerobic. <br /> • The average nitrate as nitrogen constituent in MW-2, 3 and 4 is 15.7 mg/L. MW-I has <br /> 12 mg/L indicating nitrate depletion, which is consistent with biodegradation in an <br /> anaerobic environment. <br /> ' * Redox potential has been consistently lowest in MW-I suggesting MW-I is near the <br /> center of the plume (Table 5). <br /> ' ❑ Redox potential measured over three years may suggest the site conditions are in <br /> an anaerobic state. <br /> ❑ Redox potential measurements from the last two quarters suggest that there is <br /> reaction between groundwater and the halo of the plume near MW-2, MW-3 and <br /> MW-4. <br /> • The groundwater temperature at the site ranges between 65° and 75°F. <br /> * The measured pH in the water table wells range between 7.3 and 7.6. <br /> The test results showed the following trends when comparing the contaminated zone to <br /> ' background conditions. <br /> • Alkalinity of the contaminated zone was enriched compared to background. This may <br /> ' be secondary evidence of aerobic biodegradation activity. <br /> • Nitrate of the contaminated zone was depleted compared to background. <br /> • Sulfate and total iron was inconclusive. <br /> ' • Oxidation-reduction potential of the contaminated zone is lower compared to <br /> background. <br /> • The measured pH in the water table wells range between 7.3 and 7.6. This pH range is <br /> conducive to maintaining aerobic biodegradation activity. <br /> • Temperature was slightly elevated in the impacted area. <br />