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多孔介质中的胶体滞留:流动停滞区域楔入和滞留的机理证实

Colloid retention in porous media: mechanistic confirmation of wedging and retention in zones of flow stagnation.

作者信息

Johnson W P, Li Xiqing, Yal Gozde

机构信息

Department of Geology and Geophysics, University of Utah, Salt Lake City, Utah 84112, USA.

出版信息

Environ Sci Technol. 2007 Feb 15;41(4):1279-87. doi: 10.1021/es061301x.

Abstract

A three-dimensional particle tracking model for colloid transport in porous media was developed that predicts colloid retention in porous media in the presence of an energy barrier via two mechanisms: (1) wedging of colloids within grain to grain contacts; (2) retention of colloids (without attachment) in flow stagnation zones. The model integrates forces experienced by colloids during transport in porous media, i.e., fluid drag, gravity, diffusion, and colloid-surface Derjaguin-Landau-Verwey-Overbeek interactions. The model was implemented for a fluid flow field that explicitly represented grain to grain contacts. The model utilized a variable time stepping routine to allow finer time steps in zones of rapid change in fluid velocity and colloid-surface interaction forces. Wedging was favored by colloid: collector ratios greater than about 0.005, with this threshold ratio increasing with decreasing fluid velocity. Retention in flow stagnation zones was demonstrated for colloid: collector ratios less than about 0.005, with this threshold decreasing with increasing fluid velocity. Both wedging and retention in flow stagnation zones were sensitive to colloid-surface interaction forces (energy barrier height and secondary energy minimum depth). The model provides a mechanistic basis for colloid retention in the presence of an energy barrier via processes that were recently hypothesized to explain experimental observations.

摘要

开发了一种用于多孔介质中胶体输运的三维粒子跟踪模型,该模型通过两种机制预测存在能量势垒时多孔介质中胶体的保留情况:(1)胶体在颗粒与颗粒接触处的楔入;(2)胶体(无附着)在流动停滞区的保留。该模型整合了胶体在多孔介质中输运过程中所经历的力,即流体阻力、重力、扩散以及胶体 - 表面的德贾金 - 朗道 - 韦弗 - 奥弗贝克相互作用。该模型针对明确表示颗粒与颗粒接触的流体流场进行了实现。该模型采用了可变时间步长程序,以便在流体速度和胶体 - 表面相互作用力快速变化的区域采用更精细的时间步长。当胶体与收集器的比例大于约0.005时,楔入作用更明显,且该阈值比例随流体速度降低而增加。当胶体与收集器的比例小于约0.005时,证明了在流动停滞区的保留情况,且该阈值随流体速度增加而降低。在流动停滞区的楔入和保留都对胶体 - 表面相互作用力(能量势垒高度和二次能量最小值深度)敏感。该模型通过最近被假设用于解释实验观测结果的过程,为存在能量势垒时胶体的保留提供了一个机理基础。

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