A la carte dissolution of rare earth elements from lateritic and karstic bauxite residues at mild pH: Toward sustainable extraction processes

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Abstract

Recovery of rare earth elements from bauxite residues of lateritic versus karstic origin was explored at a pH ranging between 2.7 and 4.5 using a mixture of citric acid and citrate in water. Dissolution yields of up to 82 % for lanthanum and 62 % for yttrium were achieved with excellent selectivity toward iron (a selectivity factor of up to 4200), the main element of bauxite residues. An experimental Box-Behnken statistical design identified the concentration of citric acid/citrate and temperature as key factors controlling the dissolution yield and selectivity of rare earth elements. Observed differences in dissolution yields and selectivity as a function of origin were attributed to differences in the speciation of rare earth elements in the two bauxite residues. It is therefore possible to draw an “à la carte” graph that identified the optimum citric acid/citrate concentrations and dissolution temperatures for dissolution yields and selectivity for the two BRs. This work provides fundamental knowledge for the future development of sustainable processes for the recovery of rare earth elements from bauxite residues derived from bauxites of different origin.

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红土和喀斯特铝土矿残渣中稀土元素在温和 pH 值条件下的自选溶解:实现可持续萃取工艺
在 pH 值介于 2.7 和 4.5 之间的条件下,使用柠檬酸和柠檬酸盐水混合物,研究了从红土和岩溶铝土残渣中回收稀土元素的问题。镧和钇的溶解率分别高达 82% 和 62%,对铝土矿残渣的主要元素铁具有极佳的选择性(选择性系数高达 4200)。实验箱-贝肯统计设计确定柠檬酸/柠檬酸盐浓度和温度是控制稀土元素溶解率和选择性的关键因素。观察到的稀土元素溶出率和选择性随产地的不同而不同,这是因为两种铝土矿残渣中稀土元素的种类不同。因此,可以绘制一张 "点菜 "图,确定两种铝土矿残渣溶解产率和选择性的最佳柠檬酸/柠檬酸盐浓度和溶解温度。这项工作为今后从不同来源的铝土矿残渣中回收稀土元素的可持续工艺的开发提供了基础知识。
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