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A Visual Insight into the Oxidation of Sulfide Minerals During Bioleaching and Chemical Leaching of a Complex Ore

机译:复杂矿石生物浸出和化学浸出过程中硫化矿物质氧化的可视化见解

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A scanning electron microscope (SEM) study was performed to provide a visual insight into the oxidation patterns of sulfide minerals during chemical and bacterial leaching of a complex ore for 3 days. The mineral grains were studied under SEM before and after bacterial and chemical leaching with or without the addition of ferrous iron to generate ferric iron in situ by bacteria or chemical oxidant (MnO2). Both mesophilic and moderately thermophilic cultures of bacteria were used in bioleaching tests. A limited oxidation of sphalerite and pyrite, similar to those in acid leaching (control), was observed to occur when no ferrous iron was added. However, the initial addition of ferrous iron into bioleaching media was shown to significantly improve the oxidation of sphalerite and pyrite. Galena was readily oxidized in the presence or absence of bacteria. Sphalerite was oxidized more extensively/selectively than chalcopyrite and pyrite, consistent with their respective nobility/electrochemical activity. Provided that chemical/biological oxidation of sphalerite was intensive, a sulfur-rich layer appeared to form on mineral surface. But, no such layer on pyrite surfaces was discernable. Supplementary bioleaching data were also provided to support SEM observations and to further elucidate the bioleaching characteristics of these sulfide phases. It can be inferred from this study that the oxidation of sulfides proceeds most discernibly via “indirect mechanism” and the generation of ferric iron by bacteria in sufficient quantity is essential for the effective oxidation of sulfide minerals.View full textDownload full textKeywordsacidophilic bacteria, bioleaching, complex sulfide, leaching, pyrite, sphaleriteRelated var addthis_config = { ui_cobrand: "Taylor & Francis Online", services_compact: "citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,more", pubid: "ra-4dff56cd6bb1830b" }; Add to shortlist Link Permalink http://dx.doi.org/10.1080/08827508.2010.482859
机译:进行了扫描电子显微镜(SEM)研究,以直观了解3天复杂矿石化学和细菌浸出过程中硫化物矿物的氧化方式。在细菌和化学浸提前后,通过添加或不添加亚铁,通过细菌或化学氧化剂(MnO 2 )原位生成三价铁,在SEM下对矿物晶粒进行了研究。细菌的嗜温和中度嗜热培养均用于生物浸出测试。当不添加亚铁时,观察到闪锌矿和黄铁矿的有限氧化,类似于酸浸(对照)中的那些。但是,最初向生物浸出介质中添加亚铁可显着改善闪锌矿和黄铁矿的氧化。有或没有细菌,方铅矿容易被氧化。与黄铜矿和黄铁矿相比,闪锌矿被更广泛/选择性地氧化,这与它们各自的贵族/电化学活性一致。如果闪锌矿的化学/生物氧化作用强烈,则在矿物表面上会形成富硫层。但是,在黄铁矿表面上没有发现这样的层。还提供了补充的生物浸出数据,以支持SEM观察并进一步阐明这些硫化物相的生物浸出特性。从这项研究中可以推断出,硫化物的氧化是通过``间接机制''最明显地进行的,而足够数量的细菌产生的三价铁对于硫化物矿物的有效氧化是必不可少的。 ,生物浸出,复杂硫化物浸出,黄铁矿,闪锌矿相关变量var addthis_config = {ui_cobrand:“泰勒和弗朗西斯在线”,servicescompact:“ citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,更多”, pubid:“ ra-4dff56cd6bb1830b”};添加到候选列表链接永久链接http://dx.doi.org/10.1080/08827508.2010.482859

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