
doi: 10.1201/b12522-16
Sulfate-reducing bacteria are ubiquitous in subsurface soils, sediments and groundwater systems. These bacteria couple the anaerobic oxidation of organic carbon (C) or hydrogen (H2) with the reduction of sulfate (SO42−). This results in the generation of sulfide; a powerful reductant that can drive the reductive dissolution of ferric (hydr)oxides.
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