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LiCl水溶液侵入疏水MFI型沸石的量热热:浓度的影响

Calorimetric Heats of Intrusion of LiCl Aqueous Solutions in Hydrophobic MFI-Type Zeosil: Influence of the Concentration.

作者信息

Ryzhikov Andrey, Dirand Céline, Astafan Amir, Nouali Habiba, Daou T Jean, Bezverkhyy Igor, Chaplais Gérald, Bellat Jean-Pierre

机构信息

Institut de Science des Matériaux de Mulhouse (IS2M), UMR 7361 CNRS, Axe Matériaux à Porosité Contrôlée (MPC), Université de Haute-Alsace, F-68100 Mulhouse, France.

Université de Strasbourg, F-67000 Strasbourg, France.

出版信息

Langmuir. 2024 Apr 30;40(17):8827-8835. doi: 10.1021/acs.langmuir.3c03931. Epub 2024 Apr 16.

Abstract

For the first time, we report calorimetric measurements of intrusion of aqueous LiCl solutions in a hydrophobic pure siliceous MFI zeolite (silicalite-1) under high pressure. Our results show that the intrusion heats are strongly dependent on the LiCl concentration. The intrusion process is endothermic for diluted solutions (molar HO/LiCl = 12) as well as for water, but it becomes exothermic for a concentration close to saturation (molar HO/LiCl = 4). Analysis of the data in the framework of wetting thermodynamics shows that besides surface wetting, other phenomena occur during intrusion, such as hydrogen-bond weakening and composition change. In all cases, water is preferentially intruded so that the intruded phase becomes more diluted than the bulk solution. In the case of the most diluted solution, only water molecules seemed to be intruded. Furthermore, silicalite-1 is shown to be very stable in the presence of LiCl solution, with no noticeable structural and textural modifications observed after intrusion.

摘要

我们首次报告了在高压下,水性LiCl溶液侵入疏水纯硅质MFI沸石(硅沸石-1)的量热测量结果。我们的结果表明,侵入热强烈依赖于LiCl浓度。对于稀释溶液(摩尔H₂O/LiCl = 12)以及水,侵入过程是吸热的,但对于接近饱和的浓度(摩尔H₂O/LiCl = 4),它变为放热。在润湿热力学框架内对数据的分析表明,除了表面润湿外,侵入过程中还发生其他现象,如氢键减弱和成分变化。在所有情况下,水优先侵入,使得侵入相变得比本体溶液更稀。在最稀释溶液的情况下,似乎只有水分子被侵入。此外,硅沸石-1在LiCl溶液存在下表现出非常稳定,侵入后未观察到明显的结构和织构变化。

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