Role of bicarbonate as a pH buffer and electron sink in microbial dechlorination of chloroethenes

• Main Authors: Delgado Anca G, Parameswaran Prathap, Fajardo-Williams Devyn, Halden Rolf U, Krajmalnik-Brown Rosa
• Format: Article
• Language: English
• Published: BMC 2012-09-01
• Series: Microbial Cell Factories
• Subjects: Acetogen; Alkalinity; Bicarbonate competition; <it>Dehalococcoides</it>; pH range; Trichloroethylene
• Online Access: http://www.microbialcellfactories.com/content/11/1/128

<p>Abstract</p> <p>Background</p> <p>Buffering to achieve pH control is crucial for successful trichloroethene (TCE) anaerobic bioremediation. Bicarbonate (HCO₃⁻) is the natural buffer in groundwater and the buffer of choice in the laboratory and at contaminated sites undergoing biological treatment with organohalide respiring microorganisms. However, HCO₃⁻ also serves as the electron acceptor for hydrogenotrophic methanogens and hydrogenotrophic homoacetogens, two microbial groups competing with organohalide respirers for hydrogen (H₂). We studied the effect of HCO₃⁻ as a buffering agent and the effect of HCO₃⁻-consuming reactions in a range of concentrations (2.5-30 mM) with an initial pH of 7.5 in H₂-fed TCE reductively dechlorinating communities containing <it>Dehalococcoides</it>, hydrogenotrophic methanogens, and hydrogenotrophic homoacetogens.</p> <p>Results</p> <p>Rate differences in TCE dechlorination were observed as a result of added varying HCO₃⁻ concentrations due to H₂-fed electrons channeled towards methanogenesis and homoacetogenesis and pH increases (up to 8.7) from biological HCO₃⁻ consumption. Significantly faster dechlorination rates were noted at all HCO₃⁻ concentrations tested when the pH buffering was improved by providing 4-(2-hydroxyethyl)-1-piperazineethanesulfonic acid (HEPES) as an additional buffer. Electron balances and quantitative PCR revealed that methanogenesis was the main electron sink when the initial HCO₃⁻ concentrations were 2.5 and 5 mM, while homoacetogenesis was the dominant process and sink when 10 and 30 mM HCO₃⁻ were provided initially.</p> <p>Conclusions</p> <p>Our study reveals that HCO₃⁻ is an important variable for bioremediation of chloroethenes as it has a prominent role as an electron acceptor for methanogenesis and homoacetogenesis. It also illustrates the changes in rates and extent of reductive dechlorination resulting from the combined effect of electron donor competition stimulated by HCO₃⁻ and the changes in pH exerted by methanogens and homoacetogens.</p>