首页> 外文期刊>Journal of Solution Chemistry >Isopiestic measurement of the osmotic coefficients of aqueous {xH(2)SO(4) plus (1-x)Fe-2(SO4)(3)} solutions at 298.15 and 323.15 K
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Isopiestic measurement of the osmotic coefficients of aqueous {xH(2)SO(4) plus (1-x)Fe-2(SO4)(3)} solutions at 298.15 and 323.15 K

机译:{xH(2)SO(4)加上(1-x)Fe-2(SO4)(3)}水溶液在298.15和323.15 K时的渗透系数的同量测量

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摘要

This study measures the osmotic coefficients of {xH(2)SO(4) + (1-x)Fe-2(SO4)(3)}(aq) solutions at 298.15 and 323.15 K that have ionic strengths as great as 19.3 mol.kg(-1), using the isopiestic method. Experiments utilized both aqueous NaCl and H2SO4 as reference solutions. Equilibrium values of the osmotic coefficient obtained using the two different reference solutions were in satisfactory internal agreement. The solutions follow generally the Zdanovskii empirical linear relationship and yield values of a(w) for the Fe-2(SO4)(3)-H2O binary system at 298.15 K that are in good agreement with recent work and are consistent with other M-2(SO4)(3)-H2O binary systems.
机译:这项研究测量了离子强度高达19.3 mol的{xH(2)SO(4)+(1-x)Fe-2(SO4)(3)}(aq)溶液在298.15和323.15 K的渗透系数.kg(-1),使用等分方法。实验同时使用氯化钠水溶液和硫酸作为参考溶液。使用两种不同的参考溶液获得的渗透系数的平衡值符合令人满意的内部协议。该解决方案通常遵循Zdanovskii经验线性关系和Fe-2(SO4)(3)-H2O二元体系在298.15 K时a(w)的屈服值,这与最近的工作很好地一致,并且与其他M- 2(SO4)(3)-H2O二元系统。

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