首页> 外文期刊>Journal of Solution Chemistry >Conversion of Parameters Among Variants of Scatchard’s Neutral-Electrolyte Model for Electrolyte Mixtures that Have Different Numbers of Mixing Terms
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Conversion of Parameters Among Variants of Scatchard’s Neutral-Electrolyte Model for Electrolyte Mixtures that Have Different Numbers of Mixing Terms

机译:具有不同混合项数的电解质混合物的Scatchard中性电解质模型变体之间的参数转换

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Various model equations are available for representing the excess Gibbs energy properties (osmotic and activity coefficients) of aqueous and other liquid mixed-electrolyte solutions. Scatchard’s neutral-electrolyte model is among the simplest of these equations for ternary systems and contains terms that represent both symmetrical and asymmetrical deviations from ideal mixing behavior when two single-electrolyte solutions are mixed in different proportions at constant ionic strengths. The usual form of this model allows from zero to six mixing parameters. In this report we present an analytical method for transforming the mixing parameters of neutral-electrolyte-type models with larger numbers of mixing parameters directly to those of models with fewer mixing parameters, without recourse to the source data used for evaluation of the original model parameters. The equations for this parameter conversion are based on an extension to ternary systems of the methodology of Rard and Wijesinghe (J. Chem. Thermodyn. 35:439–473, 2003) and Wijesinghe and Rard (J. Chem. Thermodyn. 37:1196–1218, 2005) that was applied by them to binary systems. It was found that the use of this approach with a constant ionic-strength cutoff of I≤6.2 mol⋅kg−1 (the NaCl solubility limit) yielded parameters for the NaCl+SrCl2+H2O and NaCl+MgCl2+H2O systems that predicted osmotic coefficients φ in excellent agreement with those calculated using the same sets of parameters whose values were evaluated directly from the source data by least-squares, with root-mean-square differences of RMSE(φ)=0.00006 to 0.00062 for the first system and RMSE(φ)=0.00014 to 0.00042 for the second. If, however, the directly evaluated parameters were based on experimental data where the ionic strength cutoff varied with the ionic-strength fraction, i.e., because they were constrained by isopiestic ionic strengths (MgCl2+MgSO4+H2O) or solubility/oversaturation ionic strengths (NaCl+SrCl2+H2O and NaCl+MgCl2+H2O), then parameters converted by this approach assuming a constant ionic-strength cutoff yield RMSE(φ) differences about an order of magnitude larger than the previous case. This indicates that for an accurate conversion of model parameters when the source model is constrained with variable ionic strength cutoffs, an extension of the parameter conversion method described herein will be required. However, when the source model parameters are evaluated at a constant ionic strength cuttoff, such as when source isopiestic data are restricted to ionic strengths at or below the solubility limit of the less soluble component, or are Emf measurements that are commonly made at constant ionic strengths, then our method yields accurate converted models.
机译:各种模型方程式可用于表示水溶液和其他液体混合电解质溶液的多余吉布斯能量性质(渗透系数和活度系数)。 Scatchard的中性电解质模型是三元体系中最简单的方程式之一,其中包含的术语代表当两种单电解质溶液以恒定的离子强度按不同比例混合时,与理想混合行为的对称偏差和非对称偏差。该模型的通常形式允许从零到六个混合参数。在此报告中,我们提出了一种分析方法,用于将具有大量混合参数的中性电解质型模型的混合参数直接转换为具有较少混合参数的模型的混合参数,而无需求助于用于评估原始模型参数的源数据。用于此参数转换的方程式基于对Rard和Wijesinghe(J. Chem。Thermodyn。35:439-473,2003)和Wijesinghe和Rard(J. Chem。Thermodyn。37:1196)方法论的扩展。 – 1218年,2005年)被他们应用于二进制系统。结果发现,采用这种方法时,离子强度的恒定截止值为I≤6.2mol⋅kg -1 (NaCl溶解度极限),可以得出NaCl + SrCl 2 <预测渗透系数φ的/ sub> + H 2 O和NaCl + MgCl 2 + H 2 O系统与使用该方法计算的渗透系数非常一致相同的参数集,其值直接通过最小二乘法从源数据中进行评估,第一个系统的均方根差为RMSE(φ)= 0.00006至0.00062,对于第一个系统,均方根误差为RMSE(φ)= 0.00014至0.00042第二。但是,如果直接评估的参数基于实验数据,其中离子强度的截断随离子强度分数而变化,即因为它们受同质离子强度(MgCl 2 + MgSO 4 + H 2 O)或溶解度/过饱和离子强度(NaCl + SrCl 2 + H 2 O和NaCl + MgCl 2 + H 2 O),然后假设恒定的离子强度截止值,通过这种方法转换的参数产生的RMSE(φ)差比以前的值大一个数量级。案件。这表明,当源模型受到可变离子强度的限制时,要进行模型参数的精确转换,将需要扩展本文所述的参数转换方法。但是,当在恒定离子强度截断值下评估源模型参数时,例如,当源同质数据仅限于处于或低于难溶成分的溶解度极限的离子强度时,或者是在恒定离子强度下通常进行的Emf测量优势,那么我们的方法就可以得出准确的转换模型。

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