首页> 外文期刊>Journal of Solution Chemistry >Isopiestic Measurement of the Osmotic Coefficients of Aqueous {xH 2 SO 4 + (1− x)Fe 2 (SO 4 ) 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 + (1− x)Fe 2 (SO 4 ) 3 } Solutions at 298.15 and 323.15 K

机译:{xH 2 SO 4 +(1-x)Fe 2 (SO 4 )3 }溶液的渗透系数的等量测量298.15和323.15 K

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This study measures the osmotic coefficients of {xH2SO4 + (1−x)Fe2(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 Fe2(SO4)3–H2O binary system at 298.15 K that are in good agreement with recent work and are consistent with other M2(SO4)3–H2O binary systems.
机译:本研究测量了{xH2 SO4 +(1-x)Fe2 (SO4 )3 }(aq)溶液在298.15和323.15处的渗透系数用等同位素方法,离子强度高达19.3 mol,kg-1 的K。实验均以NaCl水溶液和H2 SO4 作为参比溶液。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。解通常遵循Zdanovskii经验线性关系和Fe2 (SO4 )3 –H2 O二元系统在298.15 K时aw 的屈服值,与最近的工作非常吻合,并且与其他M2 (SO4 )3 –H2 O二元系统一致。

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