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A Thermodynamic Study of the Reduction of a Limonitic Laterite Ore by Methane

机译:甲烷还原褐铁矿的热力学研究

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The recovery of nickel from the oxidic nickeliferous laterite ores is receiving increasing attention due to the difficulty of recovering this metal from the sulphide ore deposits. One possible solution is to selectively reduce the nickel oxide in the ore, which could then be upgraded by, for example, magnetic concentration. In this article, a thermodynamic study was performed on the reduction of a limonitic laterite ore by methane. Methane was selected as the reducing agent as it has a lower environmental impact than carbon due to the reduced carbon dioxide emissions. The effects of temperatures and methane additions on the nickel recovery and nickel grade were investigated. High recoveries of over 95?% were predicted, but the grades were limited to about 2.5?% due to the formation of magnetite. The thermodynamic simulations for reduction by methane were in agreement with the experimental results in the literature for other reducing agents, reflecting the fact that the nickel oxide in the limonitic ore is relatively unstable. Thus, high recoveries could be achieved irrespective of the reducing agent involved.
机译:由于难以从硫化物矿床中回收这种金属,因此从氧化性含镍红土矿石中回收镍受到越来越多的关注。一种可能的解决方案是有选择地还原矿石中的氧化镍,然后可以通过例如磁性浓缩来提纯。在本文中,进行了热力学研究,研究了甲烷对氧化铁皮红土矿石的还原作用。选择甲烷作为还原剂是因为由于减少了二氧化碳的排放,甲烷对环境的影响比碳低。研究了温度和甲烷添加量对镍回收率和镍品位的影响。预计可回收率超过95%,但由于形成磁铁矿,该品位被限制在约2.5 %%。甲烷还原的热力学模拟与文献中其他还原剂的实验结果相符,反映出氧化铁皮矿石中的氧化镍相对不稳定的事实。因此,无论所涉及的还原剂如何,都可以实现高回收率。

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