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- W2912921286 abstract "Weathered crust elution-deposited rare earth ores (WREO) are the most important mineral sources of the middle and heavy rare earth in the world, which are rare earth ions (RE3+) adsorbed on clay minerals, such as montmorillonite, kaolinite, etc. In this work, the adsorption mechanism of Lanthanum ion (La3+) and Yttrium ion (Y3+) on montmorillonite was studied to clarify the interaction between RE3+ and clay minerals. The effect of aluminum ion (Al3+) on the adsorption behavior of La3+ and Y3+ was discussed, for the first time, to probe the role of Al3+ in aqueous solution and released from clay minerals. With the addition of Al3+ in solution, the adsorption capacity of RE3+ becomes much lower than that in the single RE3+ adsorption system, which indicates the inhibiting effect of Al3+ on the RE3+ adsorption. No distinct variation on the adsorption capacity of RE3+, and hence the more adsorbing sites occupied by Al3+ than RE3+ were observed at different molar concentration ratio of RE3+:Al3+ in rare earth (RE)–aluminum (Al) system. Nevertheless, there is a convert of Al3+ from adsorption to release at the molar concentration ratio from 1:5 to 1:2 of RE3+:Al3+ in RE–Al system due to the increasing initial concentration of Al3+. Kinetic studies display that the pseudo second-order kinetic model can best describe the RE3+adsorption and the Al3+release, and the two processes are controlled by chemical reaction." @default.
- W2912921286 created "2019-02-21" @default.
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- W2912921286 date "2019-02-08" @default.
- W2912921286 modified "2023-09-26" @default.
- W2912921286 title "Lanthanum (Ⅲ) and Yttrium (Ⅲ) Adsorption on Montmorillonite: The Role of Aluminum Ion in Solution and Minerals" @default.
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- W2912921286 doi "https://doi.org/10.1080/08827508.2019.1575215" @default.
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