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Okamoto, Takuya*; Okubo, Takahiro*; Iwadate, Yasuhiko*; Deguchi, Kenzo*; Shimizu, Tadashi*; Oki, Shinobu*; Tachi, Yukio
no journal, ,
The structures of Cs adsorption on montmorillonite were investigated by the nuclear magnetic resonance (NMR) spectroscopy. The NMR spectra of Cs adsorbed montmorillonite samples with different Cs contents were collected by Cs Magic Angle Spinning (MAS) NMR and Cs Triple Quantum (3Q) MAS NMR. The adsorbed Cs structures were evaluated based on the correlations between the structural characteristics and the values of the NMR parameters predicted by the first principal calculations.
Okamoto, Takuya*; Okubo, Takahiro*; Iwadate, Yasuhiko*; Deguchi, Kenzo*; Shimizu, Tadashi*; Oki, Shinobu*; Tachi, Yukio
no journal, ,
The structures of Cs adsorbed on montmorillonite were investigated by Cs Magic Angle Spinning (MAS) NMR spectroscopy. The NMR spectra of Cs adsorbed on montmorillonite samples were measured under different relative humidity levels and were analyzed to evaluate the change in the structure of hydrated Cs sorbed on montmorillonite.
Takei, Koyo*; Okubo, Takahiro*; Tachi, Yukio; Fukatsu, Yuta
no journal, ,
Cs adsorption sites on vermiculite clays were investigated by Cs magic-angle-spinning nuclear magnetic resonance (MAS NMR) and theoretical Cs chemical shift calculations. A partially Cs exchanged vermiculite sample was prepared. Three peaks on Cs MAS NMR spectra were experimentally observed. However, Cs absorption sites were not assigned to these peaks. A molecular model of fully Cs exchanged vermiculite was built to obtain Cs chemical shift theoretically by GIPAW method. Calculated Cs chemical shift ranged 23 to 47 ppm, which corresponds to the peak of the lowest field side. Detailed relationships between structure and Cs chemical shifts were investigated from Cs position and vermiculite layer structure.