Department of Chemical and Materials Engineering , University of Alberta , Edmonton , Alberta T6G 1H9 , Canada.
J Phys Chem B. 2019 Feb 7;123(5):1099-1107. doi: 10.1021/acs.jpcb.8b09285. Epub 2019 Jan 23.
The main goal of this paper is to compare the general polynomial forms of the osmotic virial equation and the Margules model for the liquid activity coefficients in binary systems. The coefficients/parameters in each model can be calculated based on best fits to experimental phase equilibrium data. Here, the activity coefficient models were combined with the equation of solid-liquid equilibrium. We obtain the coefficients/parameters for the osmotic virial equation and the one- and two-parameter Margules models and compare the accuracy of each model for fitting the experimental data for five water/solute systems: water/glycerol, water/acetic acid, water/propanoic acid, water/mono-ethylene glycol, and water/sulfolane. In obtaining the osmotic virial coefficients, we present a method to fit the equation to the entire range of data including both the ice-formation region and the solute-precipitation region. In expression of the concentration effect of the solute, we showed that the integration constant that arises from the Gibbs-Duhem equation is dependent on the osmotic virial coefficients. The osmotic virial equation is of great interest for its ability to empirically model a very wide range of aqueous solutions and as such is one of the most widely used solution models in biology.
本文的主要目的是比较渗透维里方程和二元体系中马居耳模型的一般多项式形式的液体活度系数。每个模型的系数/参数可以根据对实验相平衡数据的最佳拟合来计算。在这里,活度系数模型与固液平衡方程相结合。我们得到了渗透维里方程和单参数、双参数马居耳模型的系数/参数,并比较了每个模型对五个水/溶质体系实验数据的拟合精度:水/甘油、水/乙酸、水/丙酸、水/一缩二乙二醇和水/环丁砜。在获得渗透维里系数时,我们提出了一种将方程拟合到包括冰形成区和溶质沉淀区在内的整个数据范围的方法。在溶质浓度效应的表示中,我们表明由吉布斯-杜恒方程产生的积分常数取决于渗透维里系数。渗透维里方程因其能够经验地模拟非常广泛的水溶液而受到极大关注,因此它是生物学中最广泛使用的溶液模型之一。