Sulfuric Acid Leaching of Ionic Rare Earth Magnesium Salt Enrichment and Removing Aluminum by MgO Precipitation

浸出(土壤学) 硫酸 降水 稀土 盐(化学) 离子键合 无机化学 化学 环境化学 矿物学 冶金 离子 环境科学 材料科学 土壤科学 土壤水分 物理 有机化学 物理化学 气象学
作者
Qiang Wang,Tao Qi,Yinliang Liu,Hongdong Yu,Limin Zhang,W. L. Zhan
出处
期刊:Minerals [Multidisciplinary Digital Publishing Institute]
卷期号:15 (2): 189-189
标识
DOI:10.3390/min15020189
摘要

Production of rare earth enrichment from the in situ leaching solution of ion-adsorbed rare earth ores greatly decreases the treatment scale and significantly reduces production energy consumption and cost. However, the generated rare earth enrichment has a high content of impurities. Further purification of rare earth is necessary. Therefore, a process comprised of sulfuric acid leaching and removing aluminum by the neutralization precipitation method to obtain the purified rare earth solution was proposed. The results of acid leaching revealed that at a sulfuric acid concentration of 1.75 mol/L, a temperature of 60 °C, a liquid–solid ratio of 5:1 mL/g, a leaching time of 0.5 h, and a stirring rate of 300 r/min, leaching efficiency of rare earth and magnesium reached 99.11% and 97.39%, respectively, while the leaching efficiencies of aluminum and silicon reached 72.91% and 55.26%, respectively. The comparison of different precipitants during the neutralization precipitation process showed that MgO was the best precipitant for the efficient removal of aluminum and low loss of rare earth. The results of removing aluminum revealed that when the final pH of the rare earth leaching solution was controlled to be 4.7, the reaction temperature was 25 °C, the slurry concentration of MgO was 0.3 mol/L, and the feeding rate of the MgO slurry was 0.5 mL/min, the removal rate of aluminum was 99.49%, and the loss rate of rare earth was 13.93%. The obtained purified rare earth solution contained 19 g/L of rare earth and less than 0.01 g/L of aluminum. Kinetic studies showed that the apparent activation energy of the aluminum removal process was 6.8 kJ/mol, indicating that the precipitation process was controlled by a mass transfer diffusion reaction.

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