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首页> 外文期刊>Journal of Chemical and Engineering Data: the ACS Journal for Data >Re-evaluation of the Thermodynamic Activity Quantities in Aqueous Solutions of Uni-univalent Alkali Metal Salts of Aliphatic Carboxylic Acids and Thallium Acetate at 25 ℃
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Re-evaluation of the Thermodynamic Activity Quantities in Aqueous Solutions of Uni-univalent Alkali Metal Salts of Aliphatic Carboxylic Acids and Thallium Acetate at 25 ℃

机译:25℃脂族羧酸和乙酸hall单价碱金属盐水溶液中热力学活性量的重新估算

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摘要

The Huckel equation, which was used in this study to correlate the experimental activities of dilute solutions of uni-univalent alkali metal salts of aliphatic carboxylic acids up to a molality of about 1 mol·kg~(-1), contains two parameters that are dependent on the electrolyte: B (closely related to the ion-size parameter a* in the Debye-Huckel equation) and b1 (the coefficient of the linear term with respect to the molality, related to the hydration numbers of the ions of the electrolyte). For thallium acetate solutions, this equation applies up to a molality of 3.5 mol·kg~(-1). In more concentrated solutions of these electrolytes, in the best case up to a molality of about 7.5 mol·kg~(-1), an extended Hiickel equation was used. It contains additionally a quadratic term with respect to the molality, and the coefficient of this term is the parameter b2. All parameter values for the Hiickel equations of lithium, sodium, and potassium acetate were determined from isopiestic data measured by Robinson for solutions of these salts against KCl solutions (J. Am. Chan. Soc. 1935, 57, 1165-1168), and all parameters for rubidium, cesium and thallium acetate solutions were obtained from the osmotic coefficients reported by Robinson for solutions of these salts (J. Am. Chem. Soc. 1937, 59, 84-90). All Huckel parameters for sodium formate, propionate, butyrate, and valerate were determined from the results of isopiestic measurements of Smith and Robinson (Trans. Faraday Soc. 1942, 38, 70-78) in which these salts were measured against KCl solutions, and the parameters for the extended Hiickel equation of potassium formate solutions were solved from the recent vapor pressure data of Beyer and Steiger (J. Chem. Eng. Data 2010, 55, 830-838). The Hiickel parameters of primary sodium and potassium salts of malonic, succinic, and adipic acids were determined from the isopiestic data measured by Stokes (J. Am. Chem. Soc. 1948, 70, 1944-1946) in which these salts were measured against NaCl solutions. The resulting parameter values were tested with the vapor pressure and isopiestic data existing in the literature for the solutions of these organic salts. Most of these data support well the recommended Hiickel parameters at least up to a molality of 3.0 mol·kg~(-1) for all of the salt solutions considered. Reliable activity and osmotic coefficients for solutions of these electrolytes can therefore be calculated using the new Hiickel equations, and they have been tabulated at rounded molalities. The activity and osmotic coefficients obtained from these equations were compared to the values suggested by Robinson and Stokes (Electrolyte Solutions, 2nd ed.; Butterworths: London, 1959), to those calculated using the Pitzer equations with the parameter values of Pitzer and Mayorga (J. Phys. Chem. 1973, 77, 2300-2308), and to those calculated using the extended Hiickel equations of Hamer and Wu (J.Phys. Chem. Ref. Data 1972, 1, 1047-1099).
机译:本研究中使用的Huckel方程将脂族羧酸的单价碱金属盐的稀释溶液的实验活性与大约1 mol·kg〜(-1)的摩尔浓度相关联,该方程包含两个参数:取决于电解质:B(与Debye-Huckel方程中的离子大小参数a *密切相关)和b1(与摩尔数有关的线性项的系数,与电解质离子的水合数有关) )。对于乙酸th溶液,该方程适用的摩尔浓度为3.5 mol·kg〜(-1)。在这些电解质的更浓溶液中,在最佳摩尔浓度为约7.5 mol·kg〜(-1)的情况下,使用了扩展的Hiickel方程。它相对于摩尔浓度还包含一个二次项,该项的系数为参数b2。锂,钠和乙酸钾的Hiickel方程的所有参数值均由罗宾逊针对这些盐相对于KCl溶液的溶液的同素数据确定(J. Am。Chan。Soc。1935,57,1165-1168),以及乙酸rub,铯和th溶液的所有参数都是从Robinson报告的这些盐溶液的渗透系数中获得的(J. Am。Chem。Soc。1937,59,84-90)。甲酸,丙酸,丁酸和戊酸钠的所有Huckel参数均由Smith和Robinson的同分异构测量结果确定(Trans。Faraday Soc。1942,38,70-78),其中这些盐是针对KCl溶液测量的,以及从Beyer和Steiger的最新蒸气压数据(J. Chem。Eng。Data 2010,55,830-838)求解甲酸钾溶液的扩展Hiickel方程的参数。丙二酸,琥珀酸和己二酸的钠盐和钾盐的Hiickel参数是根据斯托克斯(J. Am。Chem。Soc。1948,70,1944-1946)测量的同构数据确定的,这些数据是根据氯化钠溶液。对于这些有机盐的溶液,使用文献中存在的蒸气压和等密度数据测试了所得的参数值。这些数据大多数都很好地支持了推荐的Hiickel参数,对于所考虑的所有盐溶液,其摩尔浓度至少为3.0 mol·kg〜(-1)。因此,可以使用新的Hiickel方程来计算这些电解质溶液的可靠活性和渗透系数,并已将它们按四舍五入的摩尔浓度制表。将从这些方程式获得的活度和渗透系数与Robinson和Stokes(《电解质溶液》,第二版; Butterworths:London,1959)建议的值进行比较,再与使用Pitzer方程式(其参数值为Pitzer和Mayorga( J. Phys。Chem。Chem。1973,77,2300-2308),以及使用Hamer和Wu的扩展Hiickel方程计算的结果(J. Phys。Chem。Ref。Data 1972,1,1047-1099)。

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