Jy. Yu et al., Solution chemistry during the lag phase and exponential phase of pyrite oxidation by Thiobacillus ferrooxidans, CHEM GEOL, 175(3-4), 2001, pp. 307-317
Pyrite was oxidised by growth of Thiobacillus ferrooxidans aerobically at 3
2 degreesC by orbital shaking at 90 revolutions per minute (rpm) in the lab
oratory. The analyses of the experimental solutions showed a long period of
adaptation (lag phase) before the onset of rapid bio-oxidation. Lag phase
lasted for approximately 400 h. During this period, the dissolved iron and
sulphur content increased very slowly compared with a very rapid rise durin
g the exponential phase of growth. The molar ratio of the dissolved Fe to S
in solution decreased from 1.3 to approximately 1 during the lag phase. Th
e molar ratio continued to fall during the exponential phase and reached ap
proximately 0.5, which is the ratio defined by the stoichiometry of pyrite.
The form of dissolved iron during the lag phase was ferrous, while during
the exponential phase, it was mostly ferric. On the other hand, all the dis
solved sulphur was in the form of SO4 during both the lag and exponential p
hase. These indicate that the Fe is preferentially leached from pyrite, but
S is the main source of energy for T. ferrooxidans during the lag phase.
The solution chemistry and scanning electron microscope images of the pyrit
e surfaces reveals that both direct and indirect leaching are important for
pyrite oxidation during the exponential phase. During the lag phase, howev
er, direct leaching appears to be the dominant mechanism, which may explain
the preferential oxidation of S during the early stages of growth. (C) 200
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