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Ion-type rare earth ore is a crucial category of strategic mineral resources in China. Rare earth elements in these ores are adsorbed on the surface of clay minerals (such as kaolinite) in the form of ion hydrate. Given the structural properties of rare earth ions and impurity ion hydrates, this study explores the mechanism of their adsorption on the surface of clay minerals. By drawing on the density functional theory, our calculations show the stable configurations of La3+ and Mg2+ hydrated ions are La(H2O)103+ and Mg(H2O)62+. We then calculated the adsorption energy, density of states, and electron transfer of La(H2O)103+ and Mg(H2O)62+ on the aluminum hydroxyl face (0 0 1) and the silica-oxygen face (0 0
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