Tm. Bhatti et al., MINERAL PRODUCTS OF PYRRHOTITE OXIDATION BY THIOBACILLUS-FERROOXIDANS, Applied and environmental microbiology, 59(6), 1993, pp. 1984-1990
The biological leaching of pyrrhotite (Fe1-xS) by Thiobacillus ferroox
idans was studied to characterize the oxidation process and to identif
y the mineral weathering products. The process was biphasic in that an
initial phase of acid consumption and decrease in redox potential was
followed by an acid-producing phase and an increase in redox potentia
l. Elemental S was one of the first products of pyrrhotite degradation
detected by X-ray diffraction. Pyrrhotite oxidation also yielded K-ja
rosite [KFe3(SO4)2(OH)6], goethite (alpha-FeOOH), and schwert-mannite
[Fe8O8(OH)6SO4] as solid-phase products. Pyrrhotite was mostly deplete
d after 14 days, whereas impurities in the form of pyrite (cubic FeS2)
and marcasite (orthorhombic FeS2) accumulated in the leach residue.