Water-assisted ionic conductance of zeolites with ZSM-5 structure

S.D. Mikhailenko , S. Kaliaguine , E. Ghali
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引用次数: 20

Abstract

The electrical conductivity (σ) of compressed powders of an isostructural series of zeolites with MFI topology1 was measured using AC impedance spectroscopy. Silicalite-1 and ZSM-5 with different Si/Al ratios containing varying numbers of Na+ and/or H+ were studied at 100% relative humidity and immersed in liquid water. In the latter case, σ is 1–2 orders of magnitude larger than that in saturated water vapour. The value of σ for silicalite immersed in water was found to be higher than that of water before and after the test. It was assumed that this is due to enhanced water dissociation on the silicalite surface. Both in water and at 100% RH the dependence of σ on cation content follows a curve with a maximum. A decrease in conductivity at a high concentration of charge carriers is ascribed to an increase in the repulsive interaction between ions in the conductive water layer on the zeolite channel walls.

ZSM-5结构沸石的水助离子电导率
采用交流阻抗谱法测定了具有MFI拓扑结构1的沸石压缩粉的电导率(σ)。硅石-1和ZSM-5具有不同的Si/Al比,含有不同数量的Na+和/或H+,并在100%相对湿度下浸泡在液态水中进行研究。后一种情况下,σ比饱和水蒸气大1 ~ 2个数量级。试验前后,硅石浸入水中的σ值均高于浸入水中的σ值。据推测,这是由于硅石表面的水解离作用增强所致。无论在水中还是在100%相对湿度下,σ对阳离子含量的依赖性都遵循一个有最大值的曲线。高浓度载流子时电导率降低的原因是沸石通道壁上导电水层中离子之间的排斥相互作用增加。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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