Pyrite and arsenopyrite concentrates were oxidized during growth of a
variety of acidophilic microorganisms over a wide temperature range. A
mesophilic culture, comprising Thiobacillus ferrooxidans and Leptospi
rillum ferrooxidans as the principal iron-oxidizing bacteria, was used
at 30 degrees C; Sulfobacillus thermosulfidooxidans was active in pur
e and mixed cultures at 48 degrees C; and Sulfolobus-like, thermoacido
philic archaea were grown at up to 84 degrees C. At low mineral concen
trations, the rate of pyrite/arsenopyrite dissolution was proportional
to temperature. However, the use of elevated temperatures to increase
rates of mineral processing over those obtainable with mesophiles app
eared to be most practicable with moderately thermophilic bacteria bec
ause growth of Sulfolobus strain BC was inhibited at higher mineral co
ncentrations. Two aspects of higher temperature bioleaching were empha
sized: the unique capacity of Sulfolobus-like archaea for extensive ch
alcopyrite oxidation; and the requirement for progress in leaching at
high mineral concentrations before the potential of these organisms ca
n be realised in process development. Copyright (C) 1996 Elsevier Scie
nce Ltd.