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基于铯固态核磁共振和密度泛函理论计算对蒙脱石黏土吸附铯的新见解

New Insights into the Cs Adsorption on Montmorillonite Clay from Cs Solid-State NMR and Density Functional Theory Calculations.

作者信息

Ohkubo Takahiro, Okamoto Takuya, Kawamura Katsuyuki, Guégan Régis, Deguchi Kenzo, Ohki Shinobu, Shimizu Tadashi, Tachi Yukio, Iwadate Yasuhiko

机构信息

Graduate School of Engineering , Chiba University , 1-33 Yayoi-cho Inage-ku , Chiba 263-8522 , Japan.

Graduate School of Environmental and Life Science , Okayama University , 1-1-1 Tsushima-naka Kita-ku , Okayama-shi , Okayama 700-8530 , Japan.

出版信息

J Phys Chem A. 2018 Dec 6;122(48):9326-9337. doi: 10.1021/acs.jpca.8b07276. Epub 2018 Nov 19.

Abstract

The adsorption sites of Cs on montmorillonite clays were investigated by theoretical Cs chemical shift calculations, Cs magic-angle-spinning nuclear magnetic resonance (MAS NMR) spectroscopy, and X-ray diffraction under controlled relative humidity. The theoretical calculations were carried out for structures with three stacking variations in the clay layers, where hexagonal cavities formed with Si-O bonds in the tetrahedral layers were aligned as monoclinic, parallel, alternated; with various d-spacings. After structural optimization, all Cs atoms were positioned around the center of hexagonal cavities in the upper or lower tetrahedral sheets. The calculated Cs chemical shifts were highly sensitive to the tetrahedral Al (Al)-Cs distance and d-spacing, rather than to the Cs coordination number. Accordingly, three peaks observed in our theoretical spectra were interpreted to be adsorbed Cs around the center of hexagonal cavity with or without Al and on the surface in the open nanospace. In a series of Cs MAS NMR spectral changes for partial Cs substituted samples, the Cs atoms are preferentially adsorbed at sites near Al for low Cs substituted montmorillonites. The presence of nonhydrated Cs was also confirmed in partially Cs substituted samples, even after being hydrated under high relative humidity.

摘要

通过理论铯化学位移计算、铯魔角旋转核磁共振(MAS NMR)光谱以及在控制相对湿度下的X射线衍射,研究了铯在蒙脱石粘土上的吸附位点。对粘土层具有三种堆积变化的结构进行了理论计算,其中四面体层中由Si - O键形成的六边形空洞排列为单斜、平行、交替排列,具有不同的d间距。结构优化后,所有铯原子都位于上层或下层四面体片层六边形空洞的中心周围。计算得到的铯化学位移对四面体铝(Al)-铯距离和d间距高度敏感,而不是对铯配位数敏感。因此,我们理论光谱中观察到的三个峰被解释为六边形空洞中心周围有或没有铝的吸附铯以及开放纳米空间表面的吸附铯。在一系列部分铯取代样品的铯MAS NMR光谱变化中,对于低铯取代的蒙脱石,铯原子优先吸附在靠近铝的位点。即使在高相对湿度下水合后,在部分铯取代样品中也证实了无水铯的存在。

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