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Electroosmotic Fluid Motion and Late-Time Solute Transort for Large Zeta Potentials

机译:大Zeta电位的电渗透流体运动和后期溶质运移

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Analytical and numerical methods are employed t o determine the electrtic potential, fluid velocity, and late-time slute distributio for electroosmotic flw in a tube and channel at #zeta# potentials tat are not necessarily small. The electric potential and fluid velocity are in general obatied by numerical means. In addiution, new anaytical solutions are presented for the velocity in a tube and chanel in the extremes of large and small Debye layer thickness. The electroosmotidc fluid velocity is used to analyze latetime transport of a neutral nonreacting xolute. Zero- and first-order solutions describing axial variatio of the solute concentration are determined analytically. The resulting expressions contain eigenvalues representing the dispersio and skewness of the axial concentration profiles. These eignenvalues and the functions describing transverse variation of the concentration field zre determined numerically using a shooting technique. Results are presented fro both tube and channel geometries over a wide range of the normalized Debye layer thickness and #zeta# potential. Simple analytical approximations to the eigenvalues are also prvided for the limiting cases of large and small values of the Deyby layer thickness.
机译:采用分析和数值方法来确定在#zeta#电位tat下管子和通道中电渗流的电势,流体速度和后期污泥分布不一定很小。电位和流体速度通常通过数值手段来满足。另外,提出了在大和小的德拜层厚度极端情况下,管子和通道中的速度的新的解析解。静电流体速度用于分析中性非反应性木酸盐的后期传输。分析确定溶质浓度轴向变化的零阶和一阶解。结果表达式包含代表轴向浓度分布的离散度和偏度的特征值。这些eignenvalues和描述浓度场z的横向变化的函数使用射击技术以数字方式确定。结果显示了在大范围归一化的德拜层厚度和#zeta#电势下,管和通道的几何形状。还为Deyby层厚度的大和小值的极限情况提供了特征值的简单分析近似值。

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