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Osmotic Pressure of Polyelectrolyte Solutions with Salt: Grand Canonical Monte Carlo Simulation Studies

机译:含盐的聚电解质溶液的渗透压:大正则蒙特卡罗模拟研究

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摘要

The thermodynamic properties of polyelectrolyte solutions are of long-standing interest. Theoretical complexity arises not only from the long-ranged electrostatic interaction but also from the multicomponent nature of the solution, In this work, we report grand canonical Monte Carlo simulations for the effect of added salt on the osmotic pressure of a primitive model of polyelectrolyte solutions. The polymer chains are freely jointed charged hard spheres, and counterions and co-ions are charged hard spheres. We use an ensemble that allows us to calculate directly the osmotic pressure for a solution in equilibrium with a bulk salt solution. As the bulk salt concentration is increased, the concentration of salt in the polyelectrolyte solution decreases and for semidilute solutions the salt concentration is very low. In dilute solution, the salt contribution to the osmotic pressure arises from electrostatic screening and excluded volume interactions. Semidilute solutions behave like salt-free solutions. The simulations show that both polymer molecules and small ions make a significant contribution to the osmotic pressure, thus questioning theories that ignore the polymer contribution. The latter effect results in the decrease in magnitude and a strong concentration dependence of the osmotic pressure. The simulation results are in qualitative accord with experiments on DNA. Scaling theories for the osmotic pressure, however, are not in agreement with the simulations or experiments.
机译:聚电解质溶液的热力学性质是长期关注的。理论上的复杂性不仅来自于长距离的静电相互作用,还来自于溶液的多组分性质。在这项工作中,我们报道了关于加盐对聚电解质溶液原始模型的渗透压影响的经典的蒙特卡洛模拟。 。聚合物链是自由连接的带电硬球,而抗衡离子和共离子是带电硬球。我们使用一个整体,可以直接计算与大量盐溶液平衡的溶液的渗透压。随着总盐浓度的增加,聚电解质溶液中盐的浓度降低,而对于半稀溶液,盐浓度非常低。在稀溶液中,盐对渗透压的贡献来自静电筛选和排除的体积相互作用。半稀释溶液的行为类似于无盐溶液。模拟表明,聚合物分子和小离子都对渗透压做出了重要贡献,因此对忽略聚合物贡献的理论提出了质疑。后一种效应导致渗透压的大小减小和强烈的浓度依赖性。仿真结果与DNA实验结果相吻合。但是,渗透压的定标理论与模拟或实验不一致。

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