Under methanogenic conditions, microbial degradation of [1,2- 14 C]vinyl chloride (VC) resulted in significant (14 ± 3% maximum recovery) but transient recovery of radioactivity as 14 C-acetate. Subsequently, 14 C-acetate was degraded to 14 CH 4 and 14 CO 2 (18 ± 2% and 54 ± 3% final recoveries, respectively). In contrast, under 2-bromoethanesulfonic acid (BES) amended conditions, 14 C-acetate recovery remained high (27 ± 1% maximum recovery) throughout the study, no 14 CH 4 was produced, and the final recovery of 14 CO 2 was only 35 ± 4%. These results demonstrate that oxidative acetogenesis may be an important mechanism for anaerobic VC biodegradation. Moreover, these results (1) demonstrate that microbial degradation of VC to CH 4 and CO 2 may involve oxidative acetogenesis followed by acetotrophic methanogenesis and (2) suggest that oxidative acetogenesis may be the initial step in the net oxidation of VC to CO 2 reported previously under Fe(III)-reducing, SO 4 -reducing, and humic acids-reducing conditions.
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Bradley et al. (2000) studied this question.
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