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首页> 外文期刊>The Journal of Chemical Thermodynamics >Water activities, osmotic and activity coefficients in aqueous chloride solutions at T = 298.15 K by the hygrometric method
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Water activities, osmotic and activity coefficients in aqueous chloride solutions at T = 298.15 K by the hygrometric method

机译:吸湿法测定T = 298.15 K时氯化物水溶液中的水分活度,渗透系数和活度系数

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Water activities of aqueous electrolyte solutions of HCl(aq), LiCl(aq), NaCl(aq), KCl(aq), CsCl(aq), NH_4Cl(aq), MgCl_2(aq), CaCl_2(aq), and Bacl_2(aq) have been determined at T = 298.15 K by the hygrometric method, and at molalities ranging from 0.2 mol(centre dot)kg~(-1) to saturation. From measurements of droplets diameters of reference NaCl(aq) or LiCl(aq), the dependence of relative humidity on solute concentrastion was determined. The data on the relative humidities allow the deduction of water activities and the osmotic coefficients at different molalities. Osmoti coefficient data have been described by the ion interaction model of Pitzer. The ion interaction parmaeters were also determined for each of the studied salts. With these parameters, the solute activity coefficients can be predicted. Our present results have been compared with reported thermodynamic data.
机译:HCl(aq),LiCl(aq),NaCl(aq),KCl(aq),CsCl(aq),NH_4Cl(aq),MgCl_2(aq),CaCl_2(aq)和Bacl_2( aq)已通过吸湿法在T = 298.15 K处测定,摩尔浓度范围为0.2 mol(中心点)kg〜(-1)至饱和。通过测量参比NaCl(aq)或LiCl(aq)的液滴直径,可以确定相对湿度对溶质浓度的依赖性。有关相对湿度的数据可以推断出不同摩尔浓度下的水分活度和渗透系数。渗透系数数据已通过Pitzer的离子相互作用模型进行了描述。还为每种研究的盐确定了离子相互作用参数。利用这些参数,可以预测溶质活度系数。我们目前的结果已与报道的热力学数据进行了比较。

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