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Reactive oxygen species generated in the presence of fine pyrite particles and its implication in thermophilic mineral bioleaching.

Authors
Type
Published Article
Journal
Applied Microbiology and Biotechnology
1432-0614
Publisher
Springer-Verlag
Publication Date
Volume
97
Issue
6
Pages
2735–2742
Identifiers
DOI: 10.1007/s00253-012-4116-y
PMID: 22584431
Source
Medline
License
Unknown

Abstract

In the tank bioleaching process, maximising solid loading and mineral availability, the latter through decreasing particle size, are key to maximising metal extraction. In this study, the effect of particle size distribution on bioleaching performance and microbial growth was studied through applying knowledge based on medical geology research to understand the adverse effects of suspended fine pyrite particles. Small-scale leaching studies, using pyrite concentrate fractions (106-75, 75-25, -25 μm fines), were used to confirm decreasing performance with decreasing particle size (D 50 <40 μm). Under equivalent experimental conditions, the generation of the reactive oxygen species (ROS), hydrogen peroxide and hydroxyl radicals from pyrite was illustrated. ROS generation measured from the different pyrite fractions was found to increase with increasing pyrite surface area loading (1.79-74.01 m(2) L(-1)) and Fe(2+) concentration (0.1-2.8 g L(-1)) in solution. The highest concentration of ROS was measured from the finest fraction of pyrite (0.85 mM) and from the largest concentration of Fe(2+) (0.78 mM). No ROS was detected from solutions containing only Fe(3+) under the same conditions tested. The potential of ROS to inhibit microbial performance under bioleaching conditions was demonstrated. Pyrite-free Sulfolobus metallicus cultures challenged with hydrogen peroxide (0.5-2.5 mM) showed significant decrease in both cell growth and Fe(2+) oxidation rates within the concentration range 1.5-2.5 mM. In combination, the results from this study suggest that conditions of large pyrite surface area loading, coupled with high concentrations of dissolved Fe(2+), can lead to the generation of ROS, resulting in oxidative stress of the microorganisms.

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