Spectroscopic analysis of the bioleaching of chalcopyrite by Acidithiobacillus caldus

被引:5
|
作者
Sasaki, Keiko [1 ]
Takatsugi, Koichiro [1 ]
Tuovinen, Olli H. [1 ,2 ]
机构
[1] Kyushu Univ, Dept Earth Resources Engn, Fukuoka 8190395, Japan
[2] Ohio State Univ, Dept Microbiol, Columbus, OH 43210 USA
关键词
Acidithiobacillus caldus; Bioleaching; Chalcopyrite; Raman spectroscopy; X-ray photoelectron spectroscopy; SULFUR; DISSOLUTION; EVOLUTION; MINERALS; SULFIDE; REACTOR; PYRITE;
D O I
10.1016/j.hydromet.2012.07.013
中图分类号
TF [冶金工业];
学科分类号
0806 ;
摘要
The formation and consumption of elemental S were investigated in the bioleaching of chalcopyrite within and without a CE dialysis membrane in Acidithiobacillus caldus cultures. The bacteria were supplemented with tetrathionate outside the membrane. XPS analysis showed that monosulfide species and elemental S were formed on CuFeS2 surface regardless of the enclosure in the dialysis membrane. They diminished over time in the inoculated systems. In the membrane enclosure, colloidal S partially dissolves and can pass the dialysis membrane for bacterial oxidation to sulfuric acid. Anaerobic pre-oxidation of CuFeS2 by Fe3+ produced S-rich deposition on mineral surface. The solubilization of Cu from membrane-enclosed pre-oxidized chalcopyrite in the A. caldus culture was much slower as compared to direct contact with bacteria. The difference is attributed to slow diffusion through the dialysis membrane as well as clogging caused by polymerized S on the inside of the membrane. (C) 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:116 / 120
页数:5
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