Re-evaluation of the Thermodynamic Activity Quantities in Pure Aqueous Solutions of Chlorate, Perchlorate, and Bromate Salts of Lithium, Sodium or Potassium Ions at 298.15 K

被引:19
作者
Partanen, Jaakko I. [1 ]
机构
[1] Lappeenranta Univ Technol, Phys Chem Lab, Dept Chem Technol, Fac Technol, Lappeenranta 53851, Finland
关键词
Activity coefficient; Osmotic coefficient; Vapor pressure; Isopiestic method; Aqueous solutions; Lithium chlorate; Lithium perchlorate; Lithium bromate; Sodium chlorate; Sodium perchlorate; Sodium bromate; Potassium chlorate; Potassium perchlorate; Potassium bromate; Critical evaluation; Debye-Huckel equation; STOICHIOMETRIC DISSOCIATION-CONSTANTS; 60; DEGREES-C; ACTIVITY-COEFFICIENT EQUATIONS; UNI-UNIVALENT ELECTROLYTES; PHTHALATE BUFFER SOLUTIONS; OSMOTIC COEFFICIENTS; CHLORIDE SOLUTIONS; PHOSPHORIC-ACID; 25-DEGREES-C; TEMPERATURES;
D O I
10.1007/s10953-012-9797-4
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The Huckel equation used to correlate the experimental activities of dilute alkali metal chlorate, perchlorate or bromate solutions up to a molality of about 1.5 mol.kg(-1) contains two electrolyte-dependent parameters: B {that is related closely to the ion-size parameter (a*) in the Debye-Huckel equation} and b(1) (this parameter is the coefficient of the linear term with respect to the molality, which is related to hydration numbers of the ions of the electrolyte). In more concentrated solutions up to 7 mol.kg(-1), an extended Huckel equation was used, it contains additionally a quadratic term with respect to the molality, and the coefficient of this term is the parameter b(2). Parameters for the Huckel equations were evaluated from isopiestic data for LiClO3, LiBrO3, LiClO4, NaClO3, NaBrO3, NaClO4, KClO3, and KBrO3. In these estimations, the Huckel parameters determined recently for NaCl solutions were used. The resulting parameter values were tested with the vapor pressure and isopiestic data available in the literature for solutions of these salts. Most of these data were reproduced within experimental error by means of the Huckel or extended Huckel equations, at least up to a molality of 3.0 mol.kg(-1), for all salts considered. Reliable activity and osmotic coefficients for solutions of these salts can, therefore, be calculated by using the new Huckel equations, and they are tabulated here at rounded molalities. The activity and osmotic coefficients obtained from these equations were compared to the values reported in several previous tabulations.
引用
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页码:271 / 293
页数:23
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