Thermodynamic model of the system H+-NH4 +-SO4 2-NO 3 --H2O at tropospheric temperatures

Simon L. Clegg, Peter Brimblecombe, Anthony S. Wexler

Research output: Journal Publications and ReviewsRGC 21 - Publication in refereed journalpeer-review

689 Citations (Scopus)

Abstract

A multicomponent mole-fraction-based thermodynamic model is used to represent aqueous phase activities, equilibrium partial pressures (of H2O, HNO3, and NH3), and saturation with respect to solid phases (H2SO4 and HNO3 hydrates, (NH4)2SO4(cr),, (NH4)3H(SO4)2(cr), NH4HSO4(cr), (NH4)2SO4·2NH4NO 3(cr) (NH4)2SO4·3NH43NH 4-NO3(cr), and NH4HSO4·NH4NO3(cr)) in the system H+-NH4 +-SO4 2--NO 3 --H2O. The model is valid from 328 to 2SO4-H2O, HNO3-H2O, and (NH4)2SO4-H2O interactions were adopted from previous studies, and values for NH4NO3-H2O obtained from vapor pressures (including data for supersaturated solutions), enthalpies, and heat capacities. Parameters for ternary interactions were determined from extensive literature data for salt solubilities, electromotive forces (emfs), and vapor pressures with an emphasis upon measurements of supersaturated H2SO4-(NH4)2SO4-H 2O solutions Comparisons suggest that the model satisfactorily represents partial pressures of both NH3 and H2SO4 above acidic sulfate mixtures in addition to that of HNO3, and salt solubilities and water activities.
Original languageEnglish
Pages (from-to)2137-2154
JournalThe Journal of Physical Chemistry A
Volume102
Issue number12
DOIs
Publication statusPublished - 19 Mar 1998
Externally publishedYes

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