铁质
矿物
三价铁
铀
硫黄
环境化学
金属
铁
化学
微生物
氧化剂
嗜热菌
铁细菌
分解
铜
冶金
细菌
矿物学
地质学
无机化学
材料科学
生物化学
有机化学
酶
古生物学
标识
DOI:10.1146/annurev.micro.56.012302.161052
摘要
▪ Abstract The use of acidiphilic, chemolithotrophic iron- and sulfur-oxidizing microbes in processes to recover metals from certain types of copper, uranium, and gold-bearing minerals or mineral concentrates is now well established. During these processes insoluble metal sulfides are oxidized to soluble metal sulfates. Mineral decomposition is believed to be mostly due to chemical attack by ferric iron, with the main role of the microorganisms being to reoxidize the resultant ferrous iron back to ferric iron. Currently operating industrial biomining processes have used bacteria that grow optimally from ambient to 50°C, but thermophilic microbes have been isolated that have the potential to enable mineral biooxidation to be carried out at temperatures of 80°C or higher. The development of higher-temperature processes will extend the variety of minerals that can be commercially processed.
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