Experimental and theoretical studies on thermodynamic activities of binaries ferric and magnesium chlorides in aqueous solutions at various temperatures

IF 2.8 3区 工程技术 Q3 CHEMISTRY, PHYSICAL
B. Makka, S.M. Aboufaris El Alaoui, K. Chakib, M. EL Guendouzi, A. Benbiyi
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Abstract

The investigation of the thermodynamic properties of binary systems of ferric and magnesium chlorides in aqueous solutions was reported at various temperatures using both the hygrometric method and thermodynamic modeling. Water activities were measured over a molality range of 0.100 up to mmax(FeCl3)= 2.500 mol·kg1 and to mmax(MgCl2)=(5.798, 6.090, 6.394, and 6.839) mol·kg1at temperatures from 298.15 K to 353.15 K, respectively. From the new measurements, the osmotic coefficients of water were evaluated and compared with the existing literature data at ambient temperature. These coefficients were treated at various temperatures using established thermodynamic models of the Pitzer, Filippov–Charykov–Rumyantsev, extended ion interaction, and Clegg–Pitzer–Brimblecombe. The relevant properties of ferric and magnesium electrolyte solutions were determined in the temperature range. Indeed, the parameterizations of FeCl3(aq) and MgCl2(aq) were evaluated and employed for the computation of solute activity and osmotic coefficients. Based on literature emf data for MgCl2(aq) at a temperature of 298.15 K, the consistency of the activity coefficients was evaluated using an adequate model, and an excellent description of the prediction activity coefficients is obtained by the extended ion interaction model. Then, the recommended activity coefficients were given at various temperatures by extending this procedure. An experimental investigation was also carried out to evaluate the solubility equilibrium of MgCl2 in aqueous solutions at different temperatures. The solubility product and standard Gibbs energies of dissolution and formation were also calculated at different temperatures and compared with those existing in the literature.

Abstract Image

不同温度下水溶液中二元氯化铁和氯化镁热力学活动的实验和理论研究
报告采用湿度法和热力学模型研究了水溶液中氯化铁和氯化镁二元体系在不同温度下的热力学性质。在 298.15 K 至 353.15 K 的温度范围内,分别测量了 0.100 至 mmax(FeCl3)= 2.500 mol-kg-1 和 mmax(MgCl2)=(5.798, 6.090, 6.394, and 6.839) mol-kg-1 的摩尔数范围内的水活度。根据新的测量结果,对水的渗透系数进行了评估,并将其与环境温度下的现有文献数据进行了比较。在不同温度下,这些系数是用已建立的 Pitzer、Filippov-Charykov-Rumyantsev、扩展离子相互作用和 Clegg-Pitzer-Brimblecombe 等热力学模型处理的。确定了铁和镁电解质溶液在该温度范围内的相关特性。事实上,对 FeCl3(aq)和 MgCl2(aq)的参数化进行了评估,并用于计算溶质活性和渗透系数。根据 MgCl2(aq)在 298.15 K 温度下的文献 emf 数据,使用适当的模型评估了活性系数的一致性。然后,通过扩展这一程序,给出了不同温度下的推荐活度系数。此外,还进行了一项实验研究,以评估不同温度下氯化镁在水溶液中的溶解平衡。此外,还计算了不同温度下的溶度积以及溶解和形成的标准吉布斯能,并与现有文献进行了比较。
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来源期刊
Fluid Phase Equilibria
Fluid Phase Equilibria 工程技术-工程:化工
CiteScore
5.30
自引率
15.40%
发文量
223
审稿时长
53 days
期刊介绍: Fluid Phase Equilibria publishes high-quality papers dealing with experimental, theoretical, and applied research related to equilibrium and transport properties of fluids, solids, and interfaces. Subjects of interest include physical/phase and chemical equilibria; equilibrium and nonequilibrium thermophysical properties; fundamental thermodynamic relations; and stability. The systems central to the journal include pure substances and mixtures of organic and inorganic materials, including polymers, biochemicals, and surfactants with sufficient characterization of composition and purity for the results to be reproduced. Alloys are of interest only when thermodynamic studies are included, purely material studies will not be considered. In all cases, authors are expected to provide physical or chemical interpretations of the results. Experimental research can include measurements under all conditions of temperature, pressure, and composition, including critical and supercritical. Measurements are to be associated with systems and conditions of fundamental or applied interest, and may not be only a collection of routine data, such as physical property or solubility measurements at limited pressures and temperatures close to ambient, or surfactant studies focussed strictly on micellisation or micelle structure. Papers reporting common data must be accompanied by new physical insights and/or contemporary or new theory or techniques.
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