Water activity and activity coefficients of the mixed electrolytes {yNH4Cl+(1−y)NH4NO3} (aq) at 298.15K

Water activities have been measured for the system {yNH4Cl+(1-y)NH4NO3+H2O}, at total electrolyte molalities from 0DDT2molkg-1to about saturation for ionic-strength fractions of NH4Cl, y=0DDT20, 0DDT50 and 0DDT80, at temperature 298DDT15K, by the hygrometric method. The obtained data allow the deduc...

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Veröffentlicht in:Fluid phase equilibria 2005-09, Vol.236 (1-2), p.205-211
Hauptverfasser: El Guendouzi, M, Errougui, A
Format: Artikel
Sprache:eng
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Zusammenfassung:Water activities have been measured for the system {yNH4Cl+(1-y)NH4NO3+H2O}, at total electrolyte molalities from 0DDT2molkg-1to about saturation for ionic-strength fractions of NH4Cl, y=0DDT20, 0DDT50 and 0DDT80, at temperature 298DDT15K, by the hygrometric method. The obtained data allow the deduction of osmotic coefficients. The experimental results are compared with the Leitzke and Stoughton rule, and Kusik and Meissner, Robinson and Stokes and Pitzer models. Good accuracy is obtained by Pitzer's model. The use of Pitzer's model involves the adjustment of the parameters D*q and D*j. The other models do not require parameter fitting. From these measurements, mixing ionic parameters are determined and used to predict the solute activity coefficients in the mixture. The obtained results are used to calculate the excess Gibbs energy at total molalities for ionic-strength fractions y.
ISSN:0378-3812
DOI:10.1016/j.fluid.2005.07.011