Collaborative effects of Acidithiobacillus ferrooxidans and ferrous ions on the oxidation of chalcopyrite
Liu, H; Lu, XC; Zhang, LJ; Xiang, WL; Zhu, XY; Li, J; Wang, XL; Lu, JJ; Wang, RC
刊名CHEMICAL GEOLOGY
2018
卷号493期号:-页码:109-120
关键词SCANNING PHOTOELECTRON MICROSCOPY SULFIDE OXIDATION SURFACE-LAYERS METAL SULFIDES MINE TAILINGS DEGREES-C COPPER IRON SULFUR PYRITE
ISSN号0009-2541
DOI10.1016/j.chemgeo.2018.05.032
文献子类期刊论文
英文摘要In recent decades, the bioleaching of chalcopyrite has been successfully developed and employed in copper hydrometallurgy. Understanding the decomposition mechanism of chalcopyrite is also of great significance for environmental remediation because the microbial oxidation of metal sulfides in mining waste and outcrop rocks commonly causes serious environmental contamination. This study investigates the influence of Acidithiobacillus ferrooxidans (A. ferrooxidans) and added Fe2+ ions on the oxidation of chalcopyrite. The results show that A. ferrooxidans and added Fe2+ ions can collaboratively promote the recovery of Cu from chalcopyrite. In the bioleaching system with added Fe2+ ions, A. ferrooxidans prefer to oxidize soluble Fe2+ ions rather than decompose chalcopyrite to acquire energy, which inhibits the release of Cu at the first stage but enhances the growth of A. ferrooxidans. After reacting for 18 days, however, the produced Fe3+ ions greatly promote decomposition and release more Cu than the bioleaching system free of Fe2+, which remained in the rest experiments. Both the oxidation of chalcopyrite and the release of Cu in the bioleaching system are greater than what occurs in the chemical leaching system. Chalcocite, covellite, bornite, and elemental sulfur were identified as intermediate products, and a sulfur transforming route of S2-/S-2(2-) -> Sn2-/S-0 -> SO32- -> SO42- can be recognized by X-ray photoelectron spectroscopy. As the principle end product, jarosite covered the chalcopyrite grains and consequently inhibited further oxidation. It is noteworthy that the released Cu2+ ions barely suppressed the growth of A. ferrooxidans because they tended to be enriched only in extracellular polymeric substance (EPS), while Fe3+ ions could be found on both the cell surfaces and the EPS, which implies a potential mechanism for the survival of cells in a high Cu2+ solution. Collectively, an integrated model of chalcopyrite oxidation, collaborated by both chemical and microbial oxidation, has been proposed to elucidate the bioleaching mechanisms and to give a perspective on its hydrometallurgical and environmental applications.
语种英语
内容类型期刊论文
源URL[http://ir.sinap.ac.cn/handle/331007/30876]  
专题上海应用物理研究所_中科院上海应用物理研究所2011-2017年
作者单位1.Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing 210023, Jiangsu, Peoples R China
2.Nanjing Univ, Sch Earth Sci & Engn, Key Lab Surficial Geochem, Minist Educ, Nanjing, Jiangsu, Peoples R China
3.Chinese Acad Sci, Shanghai Inst Appl Phys, Shanghai Synchrotron Radiat Facil, Shanghai 201204, Peoples R China
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GB/T 7714
Liu, H,Lu, XC,Zhang, LJ,et al. Collaborative effects of Acidithiobacillus ferrooxidans and ferrous ions on the oxidation of chalcopyrite[J]. CHEMICAL GEOLOGY,2018,493(-):109-120.
APA Liu, H.,Lu, XC.,Zhang, LJ.,Xiang, WL.,Zhu, XY.,...&Wang, RC.(2018).Collaborative effects of Acidithiobacillus ferrooxidans and ferrous ions on the oxidation of chalcopyrite.CHEMICAL GEOLOGY,493(-),109-120.
MLA Liu, H,et al."Collaborative effects of Acidithiobacillus ferrooxidans and ferrous ions on the oxidation of chalcopyrite".CHEMICAL GEOLOGY 493.-(2018):109-120.
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