首页> 外文会议>TMS Annual Meeting Exhibition >MICROBIAL REDUCTION OF LATERITIC NICKEL ORE FOR ENHANCED RECOVERY OF NICKEL AND COBALT THROUGH BIO-HYDROMETALLURGICAL ROUTE
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MICROBIAL REDUCTION OF LATERITIC NICKEL ORE FOR ENHANCED RECOVERY OF NICKEL AND COBALT THROUGH BIO-HYDROMETALLURGICAL ROUTE

机译:通过生物氢冶金途径增强镍和钴的微生物减少

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Present study is about use of a group of Iron[Te(III)] Reducing Bacteria (IRB) to convert the goethite (α-FeOOH) present in the original lateritic Nickel ore to magnetite under an anaerobic condition and subsequently release the bound Co(III) and Ni(II) through leaching. The lateritic Nickel ore contains 0.8% Ni, 0.049% Co, 1.92% Cr, 0.32% Mn and 50.2% Fe. An anaerobic dissimilatory Fe(III) reducing bacterial consortium capable of using acetate as carbon source (electron donor) and lateritic ore as terminal electron acceptor, changes the initial light brown color of the ore to dark brown. The change in color is due to the conversion of goethite to magnetite, which was confirmed by XRD. When the IRB treated sample was subjected to both bioleaching and acid leaching, it shows a greater recovery of Nickel and Cobalt values as compared to untreated original lateritic Ni ore. Further a magnetic separation method was used to separate the magnetic part of the treated lateritic ore and subjected to acid- and bio-leaching for better recovery of Nickel and Cobalt.
机译:目前的研究是关于使用一组铁[Te(iii)]还原细菌(IRB)在厌氧条件下将原始的后镍矿石矿石中存在的霉菌(α-FeO​​H)转化为磁铁矿,随后释放结合的CO( III)和NI(II)通过浸出。外形镍矿含有0.8%Ni,0.049%Co,1.92%Cr,0.32%Mn和50.2%Fe。减少能够使用醋酸碳作为碳源(电子供体)和外侧矿石作为终端电子受体的细菌聚集性,将矿石的初始浅棕色颜色变为深棕色。颜色的变化是由于通过XRD确认的磁石转化为磁铁矿。当对IRB处理的样品进行生物浸渍和酸浸出时,与未处理的原始乳酸Ni矿石相比,它显示出镍和钴值的更大恢复。此外,使用磁性分离方法来分离经处理的外形矿石的磁性部分,并进行酸和生物浸出,以便更好地恢复镍和钴。

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