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A View on Thermodynamics of Concentrated Electrolytes: Modification necessity for Electrostatic Contribution of Osmotic Coefficient

机译:浓缩电解质热力学的视图:渗透系数静电贡献的修饰必要性

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Prediction of the osmotic coefficient of concentrated electrolytes is needed in a wide variety of industrial applications. There is a need to correctly segregate the electrostatic contribution to osmotic coefficient from nonelectrostatic contribution. This is achieved in a rational way in this work. Using the Robinson-Stokes-Glueckauf hydrated ion model to predict non-electrostatic contribution to the osmotic coefficient, it is shown that hydration number should be independent of concentration so that the observed linear dependence of osmotic coefficient on electrolyte concentration in high concentration range could be predicted. The hydration number of several electrolytes (LiCl, NaCl, KC1, MgCl_2, and MgSO_4) has been estimated by this method. The hydration number predicted by this model shows correct dependence on temperature. It is also shown that the electrostatic contribution to osmotic coefficient is underpredicted by the Debye-Hückel theory at concentration beyond 0.1m. The Debye-Hückel theory is modified by introducing a concentration dependent hydrated ionic size. Using the present analysis, it is possible to correctly estimate the electrostatic contribution to the osmotic coefficient, beyond the range of validation of the D-H theory. This would allow development of a more fundamental model for electrostatic interaction at high electrolyte concentrations.
机译:在各种工业应用中需要预测浓缩电解质的渗透系数。需要正确地将静电系数分离到渗透系数的静电贡献。这是以合理的方式实现的。使用Robinson-Stokes-glueckauf水合离子模型来预测渗透系数的非静电贡献,表明水合数应与浓度无关,使得观察到渗透系数对高浓度范围内电解质浓度的线性依赖性可以是预料到的。通过该方法估计了几种电解质(LiCl,NaCl,KC1,MgCL_2和MgSO_4)的水合次数。通过该模型预测的水合数显示了对温度的正确依赖性。还表明,对渗透系数的静电贡献被Debye-Hückel理论以超过0.1米的浓度的脱义理论造成的。通过引入浓度依赖性水合离子尺寸来修饰Debye-Hückel理论。使用本分析,可以正确地估计渗透系数的静电贡献,超出D-H理论的验证范围。这将允许在高电解质浓度下施加静电相互作用的更基本模型。

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