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有色金属(冶炼部分):2018,(10):36-40
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离子型稀土矿硫酸镁柱浸过程中水、稀土和硫酸镁的平衡研究
王瑞祥,郭跃东,方壮,陈芳会,余攀,徐志峰*
(江西理工大学 冶金与化学工程学院,江西理工大学 冶金与化学工程学院,江西理工大学 冶金与化学工程学院,江西理工大学 冶金与化学工程学院,浙江华友钴业股份有限公司,江西理工大学 冶金与化学工程学院)
Equilibrium of Water, Rare Earth and Magnesium Sulfate in Column Leaching Process of Ion-Absorbed Rare Earth Deposits
Wang Ruixiang,Guo Yuedong,Fang zhuang,Chen fanghui,Yu Pan and Xu zhifeng*
(School of Metallurgical and Chemical Engineering,Jiangxi University of Science and Technology,Jiangxi Ganzhou,,,,,)
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投稿时间:2018-05-05     修订日期:2018-05-21     录用日期:2018-05-22     网络发布日期:2018-09-19
中文摘要: 采用柱浸方法研究无氨浸矿剂硫酸镁浸出离子型稀土矿,考察了浸矿过程中H2O、REO、Mg2 、SO2- 4走向。结果表明,每千克稀土原矿吸水量约为344 mL,稀土元素浸出率在99%以上,全过程损失率仅为0.045%,有0.24%的镁离子残留于矿体中,浸出液中镁离子总量增加4.7%,平衡率为98.76%,硫酸根总体升高0.52%。硫酸镁作为浸取剂,杂质Fe、Si的浸出率分别由硫酸铵浸矿时的0.435%、0.703%降低到0.03%、0.13%,杂质Al的浸出率基本保持不变。
中文关键词: 硫酸镁  离子型稀土矿  柱浸  浸出率  平衡率
Abstract:Ionic type rare-earth ore was column leached with ammonia magnesium sulfate leaching. Equilibrium of H2O, REO, Mg2 , and SO2- 4 during leaching was investigated. The results show that water absorbing capacity of rare earth ore is about 344 mL/kg. Leaching rate of rare earth elements is 99% above with loss rate of only 0.045% during the whole process. 0.24% magnesium ions residue exists in orebody, amount of magnesium ions in leaching solution rises 4.7% with balance rate of 98.76%. SO2- 4 rises by 0.52%. Leaching rates of impurities Fe and Si drop from 0.435% and 0.703% with ammonium sulfate as leaching agent to 0.03% and 0.13% respectively with magnesium sulfate as leaching agent, while leaching rate of impurities Al remains unchanged.
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基金项目:江西省教育厅科技项目(GJJ170489);赣州市科技局项目(赣市财教字[2017]179号)
引用文本:
王瑞祥,郭跃东,方壮,陈芳会,余攀,徐志峰.离子型稀土矿硫酸镁柱浸过程中水、稀土和硫酸镁的平衡研究[J].有色金属(冶炼部分),2018(10):36-40.
Wang Ruixiang,Guo Yuedong,Fang zhuang,Chen fanghui,Yu Pan,XUzhi-feng.Equilibrium of Water, Rare Earth and Magnesium Sulfate in Column Leaching Process of Ion-Absorbed Rare Earth Deposits[J].Nonferrous Metals (Extractive Metallurgy),2018(10):36-40.

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