Examination of the Kinetics of Bacterial Pyrite Decomposition, An

Experiment shows that the microbial degradation of pyrite does not necessarily proceed stoichiometrically. Under some conditions sulfur is oxidized preferentially leaving something approaching iron in composition; under others, the pyrite is converted almost to elemental sulfur. A kinetic model for the process based on three elementary biochemical reactions can explain these observations. The diffusion of sulfur along grain boundaries and dislocations in the solid pyrite uncouples the oxidation rates of sulfur and iron from the requirements of stoichiometry. This mechanism also explains qualitatively why bacteria adsorb preferentially at dislocation sites on pyrite surfaces, why they form "pits" at these sites, and why amorphous pyrite is more readily degraded than pure crystals. The rate-limiting step for pyrite oxidation is discussed