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Localization of cesium on montmorillonite surface investigated by frequency modulation atomic force microscopy

机译:调频原子力显微镜研究铯在蒙脱土表面的定位

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Cation exchange of clay mineral is typically analyzed without microscopic study of the clay surfaces. In order to reveal the distribution of exchangeable cations at the clay surface, we performed in situ atomic-scale observations of the surface changes in Na-rich monttnorillonite due to exchange with Cs cations using frequency modulation atomic force microscopy (FM-AFM). Lines of protrusion were observed on the surface in aqueous CsCl solution. The amount of Cs of the montmorillonite particles analyzed by energy dispersive X-ray spectrometry was consistent with the ratio of the number of linear protrusions to all protrusions in the FM-AFM images. The results showed that the protrusions represent adsorbed Cs cations. The images indicated that Cs cations at the surface were immobile, and their occupancy remained constant at 10% of the cation sites at the surface with different immersion times in the CsCl solution. This suggests that the mobility and the number of Cs cations at the surface are controlled by the permanent charge of montmorillonite; however, the Cs distribution at the surface is independent of the charge distribution of the inner silicate layer. Our atomic-scale observations demonstrate that surface cations are distributed in different ways in montmorillonite and mica. (C) 2017 Elsevier B.V. All rights reserved.
机译:通常在不对粘土表面进行微观研究的情况下分析粘土矿物的阳离子交换。为了揭示可交换阳离子在粘土表面的分布,我们使用调频原子力显微镜(FM-AFM)对富含Na的蒙脱石中由于与Cs阳离子交换而引起的表面变化进行了原位原子尺度的观察。在CsCl水溶液中的表面观察到突出线。通过能量色散X射线光谱法分析的蒙脱石颗粒的Cs的量与FM-AFM图像中线性突起与所有突起的数量之比一致。结果表明,这些突起代表吸附的Cs阳离子。图像表明表面的Cs阳离子是不动的,并且在CsCl溶液中的浸入时间不同时,它们的占据率保持在表面阳离子位置的10%不变。这表明表面的Cs阳离子的迁移率和数量受蒙脱石的永久电荷控制。然而,表面的Cs分布与内部硅酸盐层的电荷分布无关。我们的原子尺度观察表明,表面阳离子在蒙脱石和云母中以不同的方式分布。 (C)2017 Elsevier B.V.保留所有权利。

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