MX-80 bentonite was characterized by XRD and FTIR in detail. The sorption of Th(IV) on MX-80 bentonite was studied as a function of pH and ionic strength in the presence and absence of humic acid/fulvic acid. The results indicate that the sorption of Th(IV) on MX-80 bentonite increases from 0 to 95% at pH range of 0–4, and then maintains high level with increasing pH values. The sorption of Th(IV) on bentonite decreases with increasing ionic strength. The diffusion layer model (DLM) is applied to simulate the sorption of Th(IV) with the aid of FITEQL 3.1 mode. The species of Th(IV) adsorbed on bare MX-80 bentonite are consisted of “strong” species \documentclass[12pt]{minimal}
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\begin{document}$$ \equiv {\text{YOHTh}}^{4 + } $$\end{document} at low pH and “weak” species \documentclass[12pt]{minimal}
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\begin{document}$$ \equiv {\text{XOTh(OH)}}_{3} $$\end{document} at pH > 4. On HA bound MX-80 bentonite, the species of Th(IV) adsorbed on HA-bentonite hybrids are mainly consisted of \documentclass[12pt]{minimal}
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\begin{document}$$ \equiv {\text{YOThL}}_{3} $$\end{document} and \documentclass[12pt]{minimal}
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\begin{document}$$ \equiv {\text{XOThL}}_{1} $$\end{document}at pH < 4, and \documentclass[12pt]{minimal}
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\begin{document}$$ \equiv {\text{XOTh(OH)}}_{3} $$\end{document} at pH > 4. Similar species of Th(IV) adsorbed on FA bound MX-80 bentonite are observed as on FA bound MX-80 bentonite. The sorption isotherm is simulated by Langmuir, Freundlich and Dubinin–Radushkevich (D–R) models, respectively. The sorption mechanism of Th(IV) on MX-80 bentonite is discussed in detail.
