Chemical Oxidation Integrated Into Bioleaching of Pyrite and Chalcopyrite Using Immobilized Biomass

Abstract

Chemical oxidation of pyrite and chalcopyrite by ferric sulfate (Fe2(SO4)3) solution and biogenic ferric iron obtained by mixed culture of isolated thermotolerant Acidithiobacillus sp. 13Zn and Leptospirilum ferriphilum CC immobilized on natural carrierszeolite and shungite was studied. Oxidation rate of sulfide minerals was estimated by the decrease of Fe 3+ (oxidant) and increase of Fe 2+ ions in the solution. It was revealed that chemical oxidation of chalcopyrite by biogenic ferric iron occurred 2-3 times more intensively than that by Fe2(SO4)3 solution. Pyrite oxidation rate by biogenic ferric iron was twice higher than that by chemical ferric iron solution. It was shown that the treatment of pyrite and chalcopyrite by biogenic ferric iron allows to increase on average 1.5 -2 times the bioleaching of iron from pyrite and iron and copper from chalcopyrite by the associations of iron and sulfur oxidizing bacteria.

Dissolution Behaviors of Minerals in Tellurium–Bismuth Ore During Oxidic–Acidic Leaching

“…Lei et al [16] employed microorganisms to bio-leach the raw tellurium-bismuth ore, and found that less than 80% of tellurium can be leached into lixivium. During the bio-leaching of sulfide, Fe 3+ plays an active and promoting role and Fe 2+ can be oxidized to Fe 3+ by bacteria [17][18][19][20]. However, the cultivation of microorganisms and the low production efficiency limit its application.…”