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Electroosmosis of Dilute Electrolyte Solutions in Microporous Media

机译:微孔介质中稀电解质溶液的电渗

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The multiphysiochemical transport in electroosmosis of dilute electrolyte solutions (<1mM) through microporous media with granular random structures has been modeled in this work by our numerical framework consisting of three steps. First, the three-dimensional microstructures of porous media are reproduced by a random generation-growth method. Then the effects of chemical adsorption and electrical dissociation at the solid-liquid interfaces are considered to determine the electrical boundary conditions, which vary with the ionic concentration, the pH, and the temperature. Finally the nonlinear governing equations for the electrokinetic transport are solved by a highly efficient lattice Poisson-Boltzmann algorithm. The simulation results indicate that the electroosmotic permeability through the granular microporous media increases monotonically with the porosity, the ionic concentration, the pH and the environmental temperature. When the surface electric potential is higher than 50 mV, the permeability increases with the electric potential exponentially. The electroosmotic permeability increases with the pH exponentially, but with the temperature linearly. The present modeling results may improve our understanding of hydrodynamic and electrokinetic transport in geophysical systems, and help guide the design of porous electrodes in micro energy systems.
机译:稀电解质溶液(<1mM)通过具有颗粒无规结构的微孔介质在电渗中的多物理化学转运已经通过我们的包括三个步骤的数值框架进行了建模。首先,通过随机世代生长法再现多孔介质的三维微观结构。然后考虑固液界面上化学吸附和电离解的影响,以确定电边界条件,该条件随离子浓度,pH和温度的变化而变化。最后,通过高效的格子Poisson-Boltzmann算法求解了电动输运的非线性控制方程。仿真结果表明,通过颗粒微孔介质的电渗渗透率随孔隙率,离子浓度,pH和环境温度的增加而单调增加。当表面电势高于50mV时,磁导率随电势成指数增加。电渗渗透率随pH呈指数增长,但随温度呈线性增长。当前的建模结果可能会增进我们对地球物理系统中流体动力和电动传输的理解,并有助于指导微能量系统中多孔电极的设计。

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