首页> 外文期刊>Zeitschrift fur Physikalische Chemie: International Journal of Research in Physical Chemistry and Chemical Physics >Activity Coefficients of Potassium Dihydrogen Phosphate in Aqueous Solutions at 25 deg C and in Aqueous Mixture of Urea and this Electrolyte in the Temperature Range 20-35 deg C
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Activity Coefficients of Potassium Dihydrogen Phosphate in Aqueous Solutions at 25 deg C and in Aqueous Mixture of Urea and this Electrolyte in the Temperature Range 20-35 deg C

机译:磷酸二氢钾在25°C的水溶液中以及在尿素和该电解质在20-35°C的温度范围内的水溶液中的活度系数

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摘要

Simple teo-parameter Huckel and Pitzer equations were determined for the calculation of the activity and osmotic coefficients of aqueous solutions of potassium dihydrogen phosphate at 25 deg C up to a molality of the saturated solution (=1.83 mol kg~(-1)). The isopiestic data measured by Stokes (1945) were used in the parameter estimations. The resulting parameter values were tested with all thermodynamic data found in the literature for this electrolyte at this temperature. In these tests it was observed, that the Huckel equation applies to the data within experimental error up to a molality of 1.0 mol kg~(-1), and the Pitzer equation applies well to the data in the molaity range 1.0-1.83 mol kg~(-1) but not very well in dilute solutions. Therefore, also a three-parameter Pitzer equation was determined that applies to all data. The activity and osmotic coefficients calculated by these three models were compared to the values suggested by Robinson and Stokes (1959) and to those calculated by the equations of Hamer and Wu (1972) and of Pitzer and Mayorga (1973) for this electrolyte. Solubility measurements of KH_2PO_4 at 20, 25, 30 and 35 deg C were made in aqueous urea solutions, and the molality of urea varied in these measurements from 0 to 2.5 mol kg~(-1). The thermodynamics of these studies were analyzed by using the Pitzer formalism. It was observed that only one interaction parameter between urea molecules and ions (this parameter is linearly dependent on the temperature) was needed to describe almost completely the new solubility data.
机译:确定简单的定理参数Huckel和Pitzer方程,以计算磷酸二氢钾在25℃至饱和溶液的摩尔浓度(= 1.83 mol kg〜(-1))的活度和渗透系数。由斯托克斯(1945)测量的等度数据用于参数估计。在此温度下,使用文献中找到的所有热力学数据测试所得的参数值。在这些测试中,可以观察到Huckel方程适用于在1.0 mol kg〜(-1)的摩尔摩尔浓度内的实验误差范围内的数据,而Pitzer方程适用于1.0-1.83 mol kg摩尔浓度范围内的数据〜(-1),但在稀溶液中不是很好。因此,还确定了适用于所有数据的三参数Pitzer方程。将这三种模型计算出的活度和渗透系数与Robinson和Stokes(1959)所建议的值以及通过Hamer和Wu(1972)以及Pitzer和Mayorga(1973)的方程所计算出的值进行比较。在尿素水溶液中于20、25、30和35℃下测量KH_2PO_4的溶解度,并且尿素的摩尔浓度在0至2.5 mol kg〜(-1)之间变化。这些研究的热力学是通过使用Pitzer形式主义进行分析的。已观察到,仅需要一个尿素分子与离子之间的相互作用参数(该参数线性依赖于温度)即可几乎完全描述新的溶解度数据。

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