Adsorption Behaviors of Lanthanum (III) and Yttrium (III) Ions on Gibbsite

被引:3
作者
Zhou, Zongke [1 ]
Wan, Quan [1 ,2 ]
Yu, Wenbin [1 ]
Nie, Xin [1 ]
Yang, Shuguang [1 ]
Yang, Shuqin [1 ]
Qin, Zonghua [1 ]
机构
[1] Chinese Acad Sci, Inst Geochem, State Key Lab Ore Deposit Geochem, Guiyang 550051, Peoples R China
[2] CAS Ctr Excellence Comparat Planetol, Hefei 230026, Peoples R China
基金
中国国家自然科学基金;
关键词
gibbsite; rare earth element; adsorption; kinetics; thermodynamics; METAL-IONS; AQUEOUS-SOLUTION; BAUXITE DEPOSIT; CLAY-MINERALS; REE; KAOLINITE; SORPTION; SPECTROSCOPY; EUROPIUM; BASIN;
D O I
10.3390/min13121530
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The enrichment process of rare earth elements in ion-adsorbed rare earth ores and bauxite is potentially related to the adsorption of rare earth elements by gibbsite. In this paper, lanthanum and yttrium were selected as surrogates of light rare earth elements and heavy rare earth elements, respectively. The effects of adsorption time, solution pH, and background electrolyte concentration on the adsorption of rare earth ions by gibbsite were investigated through batch adsorption experiments. The results showed that the adsorption of rare earth ions by gibbsite can approach equilibrium in 72 h. There is mainly electrostatic repulsion between gibbsite and rare earth ions at pH 4-7, and the adsorption efficiency increases with the increase in solution pH value and background electrolyte concentration. The adsorption process of rare earth ions by gibbsite is more consistent with the pseudo-second-order kinetic and Langmuir single-layer adsorption models. Moreover, based on the structural correlation between clay minerals and gibbsite, the causes for the differences in the adsorption behaviors of rare earth elements on the minerals are discussed. The results of this study help to understand the role of aluminum hydroxide in the migration and fate of rare earth elements in epigenetic environments.
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页数:12
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