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Thermodynamics of ions precipitation in mixed-solvent mixtures

机译:混合溶剂混合物中离子沉淀的热力学

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A framework derived from thermodynamic principles of solid-liquid equilibrium criteria was formulated to correlate and predict the precipitation of salts from aqueous solutions using organic solvents. The activity coefficient of a given salt in a mixed-solvent mixture was related to the activity coefficients of such a salt in each of the pure solvents (water and organic) using the excess Henry's constant approach (H~E_i). The Wohl's expansion was then employed to model the excess Gibbs free energy (g~E) function. Two equations were provided; the two-suffix equation, and the three-suffix equation. A previously acquired precipitation database was used to evaluate the correlative ability of the framework equations. The precipitation measurements were adequately correlated and predicted by the two interaction parameters equation; the two-suffix equation. However, the three-suffix equation, with three interaction parameters, was more accurate. The regressed interaction parameters can be used as predictive tools to estimate the precipitation fractions (P) for the tested systems for which no experimental data are available. Furthermore, such parameters can be employed to predict the solubilities of the tested salts in the organic solvent.
机译:制定了从固液平衡标准的热力学原理得出的框架,以关联和预测使用有机溶剂从水溶液中沉淀出的盐。使用过量亨利常数方法(H〜E_i),给定盐在混合溶剂混合物中的活度系数与该盐在每种纯溶剂(水和有机物)中的活度系数相关。然后,用Wohl展开来模拟多余的吉布斯自由能(g〜E)函数。提供了两个方程式;两个后缀方程式和三个后缀方程式。使用先前获得的降水量数据库来评估框架方程的相关能力。通过两个相互作用参数方程对降水量进行了充分的关联和预测。两个后缀的方程式。但是,具有三个交互参数的三后缀方程更为精确。回归的相互作用参数可以用作预测工具,以估计没有实验数据的被测系统的降水分数(P)。此外,这些参数可以用来预测被测盐在有机溶剂中的溶解度。

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