Determination of Hansen Solubility Parameters of Raw Muscovite

IF 2 4区 地球科学 Q4 CHEMISTRY, PHYSICAL
Ming Weng, Xiuhua Wang
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Abstract

Muscovite has been used increasingly as a substrate in flexible electronics and fillers in high-performance nanocomposites. Muscovite-based interfacial interactions play a crucial rule in material fabrication. Hansen solubility parameters (HSPs) have proven useful in characterizing molecular interactions within/between condensed phases. The present study aimed to determine the HSPs of raw muscovite (RM) and to investigate solvent dispersion mechanisms of RM. To achieve this, the solubilities of RM in 17 solvents were evaluated by dispersion tests, and the HSPs of RM were calculated as the center of the optimal solubility rotated-ellipsoid in HSP space, which included all good solvents, had the smallest number of outliers, and had the smallest volume. The resulting dispersion, polar, and hydrogen bonding components of RM were 18.301, 2.366, and 3.727 MPa1/2, respectively. By considering the HSPs and Kamlet-Taft's solvatochromic parameters of solvents, we concluded that the low polarity of RM is due to hindered K+/H+ exchange on the RM surface, resulting from limited water/moisture contact. For solvent dispersion of RM, essential conditions include strong dispersion forces and weak polar forces, finely tuned to match the surface property of RM at a certain hydration level. The HSPs of RM determined from dispersion tests were restricted to predicting/characterizing RM-based interfacial phenomena in an environment with strictly controlled water/moisture content. The HSP calculation method proposed herein was applicable to any clay mineral.

Abstract Image

测定未加工云英岩的汉森溶解度参数
白云母越来越多地用作柔性电子器件的衬底和高性能纳米复合材料的填料。基于莫斯科的界面相互作用在材料制造中起着至关重要的作用。汉森溶解度参数(HSPs)在表征缩合相内部/之间的分子相互作用方面已被证明是有用的。本研究旨在测定生白云母(RM)的热敏感蛋白,并探讨其溶剂分散机制。为了实现这一目标,通过分散试验评价了RM在17种溶剂中的溶解度,并计算了RM的HSPs作为HSP空间中最佳溶解度旋转椭球的中心,该空间包括所有良好的溶剂,异常值最少,体积最小。结果表明,RM的色散、极性和氢键组分分别为18.301、2.366和3.727 MPa1/2。通过考虑溶剂的HSPs和Kamlet-Taft溶剂致变色参数,我们得出RM的低极性是由于RM表面的K+/H+交换受阻,这是由于有限的水/湿接触造成的。对于RM的溶剂分散,必要条件包括强分散力和弱极性力,微调以匹配RM在一定水化水平下的表面性质。在严格控制水/水分含量的环境下,从分散试验中确定的RM的热敏感值仅限于预测/表征基于RM的界面现象。本文提出的热稳定性计算方法适用于任何粘土矿物。
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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来源期刊
Clays and Clay Minerals
Clays and Clay Minerals 地学-地球科学综合
CiteScore
3.40
自引率
9.10%
发文量
46
审稿时长
3 months
期刊介绍: Clays and Clay Minerals aims to present the latest advances in research and technology concerning clays and other fine-grained minerals, including but not limited to areas in agronomy, ceramics, colloid chemistry, crystallography, environmental science, foundry engineering, geochemistry, geology, medicinal chemistry, mineralogy, nanoscience, petroleum engineering, physical chemistry, sedimentology, soil mechanics, and soil science. Clays and Clay Minerals exists to disseminate to its worldwide readership the most recent developments in all of these aspects of clay materials. Manuscripts are welcome from all countries.
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