Conventional anaerobic digestion emits methane from organic waste. Here, we investigate a sulfate-based alternative that suppresses methane production and generates alkaline solutions that may sequester carbon by carbonate precipitation. Although methanogenesis is known to occur when reduced organic carbon is replete and sulfate is limiting, it remains unclear whether methane emissions during microbial conversion of waste gypsum are primarily driven by community composition or organic availability. By comparing fluxes of electrons from organic matter toward sulfate or methane in microbial communities grown on different organic loads, we show that community composition, microbial growth, and organic availability collectively determine sulfide and methane fluxes. Lower organic loads increase the importance of syntrophic interactions with fermenters and competition between sulfate reducing bacteria and methanogens due to scarcity of substrates. Microbes present in the original sewage sludge reduce less sulfate, produce more methane, and generate less alkalinity compared to the communities enriched by multiple cycles of growth in the presence of sulfate and sewage sludge. The inoculation of communities enriched at low organic loadings in the presence of sulfate decreases the production of methane by enabling the growth of sulfate reducing bacteria from the order Desulfobacterales that can oxidize acetate to CO2 and compete with methanogens for acetate. The use of such enrichments in sludge treatment systems can stimulate the removal of organic substrates and waste gypsum, while suppressing methane production, over timescales comparable to those in the current sludge treatment systems that do not contain sulfate.
Coon, G. R., Kouadio, V., Murphy, C. W. M., Sun, H., Jagoutz, O., Bosak, T.
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