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重力作用下扩散电泳胶体悬浮液的单向干燥

Unidirectional drying of a suspension of diffusiophoretic colloids under gravity.

作者信息

Xu Jinjie, Wang Zhikui, Chu Henry C W

机构信息

Department of Chemical Engineering, University of Florida Gainesville FL 32611 USA

出版信息

RSC Adv. 2023 Mar 20;13(14):9247-9259. doi: 10.1039/d3ra00115f.

Abstract

Recent experiments (K. Inoue and S. Inasawa, , 2020, , 15763-15768) and simulations (J.-B. Salmon and F. Doumenc, , 2020, , 024201) demonstrated the significant impact of gravity on unidirectional drying of a colloidal suspension. However, under gravity, the role of colloid transport induced by an electrolyte concentration gradient, a mechanism known as diffusiophoresis, is unexplored to date. In this work, we employ direct numerical simulations and develop a macrotransport theory to analyze the advective-diffusive transport of an electrolyte-colloid suspension in a unidirectional drying cell under the influence of gravity and diffusiophoresis. We report three key findings. First, drying a suspension of solute-attracted diffusiophoretic colloids causes the strongest phase separation and generates the thinnest colloidal layer compared to non-diffusiophoretic or solute-repelled colloids. Second, when colloids are strongly solute-repelled, diffusiophoresis prevents the formation of colloid concentration gradient and hence gravity has a negligible effect on colloidal layer formation. Third, our macrotransport theory predicts new scalings for the growth of the colloidal layer. The scalings match with direct numerical simulations and indicate that the colloidal layer produced by solute-repelled diffusiophoretic colloids could be an order of magnitude thicker compared to non-diffusiophoretic or solute-attracted colloids. Our results enable tailoring the separation of colloid-electrolyte suspensions by tuning the interactions between the solvent, electrolyte, and colloids under Earth's or microgravity, which is central to ground-based and in-space applications.

摘要

最近的实验(K. 井上和 S. 稻泽,《》,2020 年,《》,15763 - 15768)和模拟(J.-B. 萨尔蒙和 F. 杜门克,《》,2020 年,《》,024201)表明重力对胶体悬浮液的单向干燥有显著影响。然而,在重力作用下,由电解质浓度梯度引起的胶体输运作用,即一种被称为扩散泳的机制,迄今为止尚未得到研究。在这项工作中,我们采用直接数值模拟并发展了一种宏观输运理论,以分析在重力和扩散泳影响下,单向干燥池中电解质 - 胶体悬浮液的平流 - 扩散输运。我们报告了三个关键发现。首先,与非扩散泳或溶质排斥型胶体相比,干燥溶质吸引型扩散泳胶体的悬浮液会导致最强的相分离,并产生最薄的胶体层。其次,当胶体强烈排斥溶质时,扩散泳会阻止胶体浓度梯度的形成,因此重力对胶体层形成的影响可忽略不计。第三,我们的宏观输运理论预测了胶体层生长的新标度律。这些标度律与直接数值模拟结果相符,表明溶质排斥型扩散泳胶体产生的胶体层可能比非扩散泳或溶质吸引型胶体厚一个数量级。我们的结果使得通过调整地球或微重力条件下溶剂、电解质和胶体之间的相互作用来定制胶体 - 电解质悬浮液的分离成为可能,这对于地面和太空应用至关重要。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5d65/10026375/487194f08af5/d3ra00115f-f1.jpg

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