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首页> 外文期刊>The Journal of Chemical Physics >Osmotic pressure acting on a semipermeable shell immersed in a solution of polyions
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Osmotic pressure acting on a semipermeable shell immersed in a solution of polyions

机译:作用在浸入多离子溶液中的半透壳上的渗透压

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We study theoretically the osmotic equilibria for a shell immersed in a suspension of polyions (e.g., colloids, polyelectrolytes, etc.). The shell is treated as impermeable for polyions, but allowing free diffusion of counterions that permeate inside the shell. From the solution of linearized Poisson-Boltzmann equation, we obtain the distribution of a potential and concentration profiles for polyions and counterions. We then obtain an explicit formula for the excess osmotic pressure of a polyion solution exerted on the shell, which includes a quadratic term in order to provide a self-consistency of a linear theory. As a result this pressure is larger than given by a concentration of polyions at the outer shell boundary obtained within linearized theory. It is, however, always smaller than or equal to the bulk osmotic pressure. This difference is attributed to a repulsive electrostatic disjoining pressure due to an overlap of counterion clouds inside the shell. A comparison with molecular dynamics simulations is provided and demonstrates that although the concentration profiles obtained within a linear theory deviate from simulation data at large potential, the theoretical and simulation pressures are in surprisingly good harmony.
机译:我们从理论上研究了浸入多离子悬浮液(例如胶体、聚电解质等)中的壳的渗透平衡。壳层被视为对聚离子不渗透,但允许渗透到壳层内部的反离子自由扩散。从线性化泊松-玻尔兹曼方程的解中,我们得到了多离子和反离子的势分布和浓度分布。然后,我们得到了施加在壳上的多离子溶液的过量渗透压的显式公式,其中包括一个二次项,以提供线性理论的自洽性。因此,该压力大于线性化理论中获得的外壳边界处的多离子浓度所给出的压力。然而,它总是小于或等于整体渗透压。这种差异归因于由于壳内反离子云重叠而导致的排斥性静电分离压力。与分子动力学模拟进行了比较,表明尽管在线性理论中获得的浓度分布在大电位下与模拟数据存在偏差,但理论压力和模拟压力却出奇地协调一致。

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