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Anaerobic Biodegradation of Chloroform and Dichloromethane with a Dehalobacter Enrichment Culture.
Wang, Hao; Yu, Rong; Webb, Jennifer; Dollar, Peter; Freedman, David L.
Afiliação
  • Wang H; Department of Environmental Engineering and Earth Sciences, Clemson Universitygrid.26090.3d, Clemson, South Carolina, USA.
  • Yu R; Synterra, Greenville, South Carolina, USA.
  • Webb J; SiREM, Guelph, Ontario, Canada.
  • Dollar P; Geosyntec Consultants International Inc., Toronto, Ontario, Canada.
  • Freedman DL; Department of Environmental Engineering and Earth Sciences, Clemson Universitygrid.26090.3d, Clemson, South Carolina, USA.
Appl Environ Microbiol ; 88(4): e0197021, 2022 02 22.
Article em En | MEDLINE | ID: mdl-34936839
ABSTRACT
Chloroform (CF) and dichloromethane (DCM) are among the more commonly identified chlorinated aliphatic compounds found in contaminated soil and groundwater. Complete dechlorination of CF has been reported under anaerobic conditions by microbes that respire CF to DCM and others that biodegrade DCM. The objectives of this study were to ascertain if a commercially available bioaugmentation enrichment culture (KB-1 Plus CF) uses an oxidative or fermentative pathway for biodegradation of DCM and to determine if the products from DCM biodegradation can support organohalide respiration of CF to DCM in the absence of an exogenous electron donor. In various treatments with the KB-1 Plus CF culture to which 14C-CF was added, the predominant product was 14CO2, indicating that oxidation is the predominant pathway for DCM. Recovery of 14C-DCM when biodegradation was still in progress confirmed that CF first undergoes reductive dechlorination to DCM. 14C-labeled organic acids, including acetate and propionate, were also recovered, suggesting that synthesis of organic acids provides a sink for the electron equivalents from oxidation of DCM. When the biomass was washed to remove organic acids from prior additions of exogenous electron donor and only CF and DCM were added, the culture completely dechlorinated CF. The total amount of DCM added was not sufficient to provide the electron equivalents needed to reduce CF to DCM. Thus, the additional reducing power came via the DCM generated from CF reduction. Nevertheless, the rate of CF consumption was considerably lower compared to that of treatments that received an exogenous electron donor. IMPORTANCE Chloroform (CF) and dichloromethane (DCM) are among the more commonly identified chlorinated aliphatic compounds found in contaminated soil and groundwater. One way to address this problem is to add microbes to the subsurface that can biodegrade these compounds. While microbes are known that can accomplish this task, less is known about the pathways used under anaerobic conditions. Some use an oxidative pathway, resulting mainly in carbon dioxide. Others use a fermentative pathway, resulting in formation of organic acids. In this study, a commercially available bioaugmentation enrichment culture (KB-1 Plus CF) was evaluated using carbon-14 labeled chloroform. The main product formed was carbon dioxide, indicating the use of an oxidative pathway. The reducing power gained from oxidation was shown to support reductive dechlorination of CF to DCM. The results demonstrate the potential to achieve full dechlorination of CF and DCM to nonhazardous products that are difficult to identify in the field.
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Texto completo: 1 Base de dados: MEDLINE Assunto principal: Clorofórmio / Cloreto de Metileno Idioma: En Ano de publicação: 2022 Tipo de documento: Article

Texto completo: 1 Base de dados: MEDLINE Assunto principal: Clorofórmio / Cloreto de Metileno Idioma: En Ano de publicação: 2022 Tipo de documento: Article