Thiobacillus ferrooxidans and the formation of acidity in simulated coal mine environments

Abstract

Laboratory simulations have helped resolve several problems concerning the role of bacteria in producing acidic drainage from active and abandoned coal mines. It is well established that the bacterium Thiobacillus ferrooxidans oxidizes pyrite in synthetic liquid media and in flooded or agitated experimental simulations of coal mine environments. However, many geologists remain skeptical regarding the role of T. ferrooxidans in producing acidity below a near‐surface belt of soil water. We have demonstrated that T. ferrooxidans is capable of colonizing and acidifying a near‐neutral pH environment of crushed coal or overburden, without prior establishment of a pH‐dependent succession of bacteria. We have suggested that T. ferrooxidans may accomplish this by direct oxidation of pyrite. We have also shown that T. ferrooxidans catalyzes pyrite oxidation in the intermediate belt of the zone of aeration, although only for a limited period of time after rainfall infiltration. T. ferrooxidans was not found to be significant in the simulated zone of groundwater saturation.