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流道中流体置换前缘引起的胶体运移。

Colloid mobilization by fluid displacement fronts in channels.

机构信息

Department of Plant and Soil Sciences, University of Delaware, Newark, DE 19716, USA.

出版信息

J Colloid Interface Sci. 2013 Sep 15;406:44-50. doi: 10.1016/j.jcis.2013.05.078. Epub 2013 Jun 7.

DOI:10.1016/j.jcis.2013.05.078
PMID:23800372
Abstract

Understanding colloid mobilization during transient flow in soil is important for addressing colloid and contaminant transport issues. While theoretical descriptions of colloid detachment exist for saturated systems, corresponding mechanisms of colloid mobilization during drainage and imbibition have not been considered in detail. In this work, theoretical force and torque analyses were performed to examine the interactive effects of adhesion, drag, friction, and surface tension forces on colloid mobilization and to outline conditions corresponding to the mobilization mechanisms such as lifting, sliding, and rolling. Colloid and substrate contact angles were used as variables to determine theoretical criteria for colloid mobilization mechanisms during drainage and imbibition. Experimental mobilization of hydrophilic and hydrophobic microspheres with drainage and imbibition fronts was investigated in hydrophilic and hydrophobic channels using a confocal microscope. Colloid mobilization differed between drainage and imbibition due to different dynamic contact angles and interfacial geometries on the contact line. Experimental results did not fully follow the theoretical criteria in all cases, which was explained with additional factors not included in the theory such as presence of aggregates and trailing films. Theoretical force and torque analyses resulted in similar mobilization predictions and suggested that all mobilization mechanisms contributed to the observed colloid mobilization.

摘要

理解土壤中瞬变流过程中的胶体迁移对于解决胶体和污染物迁移问题非常重要。虽然已有关于饱和系统中胶体脱离的理论描述,但在排水和吸渗过程中胶体迁移的相应机制尚未得到详细考虑。在这项工作中,进行了理论力和力矩分析,以研究粘附力、阻力、摩擦力和表面张力对胶体迁移的相互影响,并概述了与提升、滑动和滚动等迁移机制相对应的条件。胶体和基质接触角被用作变量,以确定排水和吸渗过程中胶体迁移机制的理论标准。使用共聚焦显微镜在亲水和疏水通道中研究了具有排水和吸渗前缘的亲水和疏水微球的实验性胶体迁移。由于接触线上的动态接触角和界面几何形状不同,排水和吸渗过程中的胶体迁移有所不同。在所有情况下,实验结果都没有完全遵循理论标准,这可以用理论中未包含的其他因素来解释,例如团聚体和拖尾膜的存在。理论力和力矩分析得出了相似的迁移预测,并表明所有迁移机制都促成了观察到的胶体迁移。

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