Table 4. Geochemical indicators of terminal electron acceptor processes measured during this study
Constituent |
Remarks concerning interpretation |
Dissolved oxygen (DO) |
If DO is greater than 1 mg/L (aerobic conditions), reductive dechlorination is unlikely; however, cometabolism and direct oxidation of partially dechlorinated solvents are possible. |
Nitrate (NO3-) |
Reductive dechlorination of tetrachloroethylene (PCE) and trichloroethylene (TCE) to cis-1,2-dichloroethylene (cDCE) can occur under these mildly reducing conditions. Direct oxidation of partially dechlorinated solvents also may occur under NO3--reducing conditions. |
Ammonia (NH3) |
Elevated NH3 concentrations may indicate NO3--reduction if DO is less than 1 mg/L. If NH3 is present at 0.5 mg/L or greater and DO levels are greater than 1.0 mg/L, then partially dechlorinated solvents may be cometabolized through the NH3-monooxygenase pathway. |
Soluble manganese (Mn2+) and ferrous iron (Fe2+). |
Increased concentrations of Mn2+ and Fe2+, coinciding with low DO concentrations, are indicators that insoluble manganese and iron (Mn4+ and Fe3+) are serving as electron acceptors. Reductive dechlorination of PCE and TCE to cDCE can occur under mildly reducing conditions. Mn4+- and Fe3+-reducing bacteria are capable of consuming vinyl chloride (VC) and cDCE. |
Sulfate (SO42-) |
Reductive dechlorination of TCE to cDCE, then to VC and ethene can occur under SO42--reducing conditions. The chlorinated solvents compete directly with SO42- to serve as electron acceptors. |
Sulfide (S2-) |
Elevated S2- concentrations may indicate SO42--reduction and conditions favorable for reductive dechlorination of chlorinated solvents. |
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