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Handbook of Solvents - George Wypych - ChemTech - Ventech!

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23.1 Natural attenuation <strong>of</strong> chlorinated solvents 1587<br />

23.1.3.2.2 Aerobic cometabolism <strong>of</strong> chlorinated compounds<br />

It has been reported that under aerobic conditions chlorinated ethenes, with the exception <strong>of</strong><br />

PCE, are susceptible to cometabolic oxidation. 30,53,81,82 Vogel 30 further elaborates that the<br />

oxidation rate increases as the degree <strong>of</strong> chlorination decreases. Aerobic cometabolism <strong>of</strong><br />

ethenes may be characterized by a loss <strong>of</strong> contaminant mass, the presence <strong>of</strong> intermediate<br />

degradation products (e.g., chlorinated oxides, aldehydes, ethanols, and epoxides), and the<br />

presence <strong>of</strong> other products such as chloride, carbon dioxide, carbon monoxide, and a variety<br />

<strong>of</strong> organic acids. 53,83 Cometabolism requires the presence <strong>of</strong> a suitable primary substrate<br />

such as toluene, phenol, or methane. For cometabolism to be effective, the primary substrate<br />

must be present at higher concentrations than the chlorinated compound, and the system<br />

must be aerobic. Because the introduction <strong>of</strong> high concentrations <strong>of</strong> oxidizable organic matter<br />

into an aquifer quickly drives the groundwater anaerobic, aerobic cometabolism typically<br />

must be engineered.<br />

23.1.3.2.3 Anaerobic oxidation <strong>of</strong> chlorinated compounds<br />

Anaerobic oxidation occurs when<br />

anaerobic bacteria use the chlorinated<br />

solvent as an electron donor<br />

by utilizing an available electron<br />

acceptor such as ferric iron<br />

(Fe(III)). Bradley and Chapelle 84<br />

show that vinyl chloride can be<br />

oxidized to carbon dioxide and<br />

water via Fe(III) reduction. In microcosms<br />

amended with<br />

Fe(III)-EDTA, reduction <strong>of</strong> vinyl<br />

chloride concentrations closely<br />

matched the production <strong>of</strong> carbon<br />

dioxide. Slight mineralization was<br />

also noted in unamended microcosms.<br />

The rate <strong>of</strong> this reaction<br />

apparently depends on the<br />

bioavailability <strong>of</strong> Fe(III). In a subsequent<br />

paper, Bradley and<br />

Chapelle 85 reported “significant”<br />

anaerobic mineralization <strong>of</strong> both<br />

DCE and VC in microcosms containing<br />

creek bed sediments. The<br />

sediments were taken from a<br />

stream where groundwater containing<br />

chlorinated ethenes con-<br />

Figure 23.1.5. Reaction sequence and relative rates for tinually discharges. Anaerobic<br />

halorespiration <strong>of</strong> chlorinated ethenes, with other reactions shown.<br />

mineralization was observed in<br />

[From T.H. Wiedemeier, H. S. Rifai, C. J. Newell and J.T. Wilson,<br />

Natural Attenuation <strong>of</strong> Fuels and Chlorinated <strong>Solvents</strong> in the both methanogenic and Fe(III) re-<br />

Subsurface, reaction rates description from reference 88. Copyright ducing conditions.<br />

© 1999 John Wiley & Sons, Inc. Reprinted by permission <strong>of</strong> John<br />

Wiley & Sons, Inc.]

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