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Thermodynamic Functions of Solutions

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Mixtures and Mineral Reactions

Part of the book series: Minerals and Rocks ((MINERALS,volume 19))

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Abstract

The chemical potential (μi and fugacity (fi) are alternative but related measures of the escaping tendency of a substance. The necessary condition of equilibrium between two phases, α and β, with respect to the diffusion of any component i, which is free to move between these phases, can be expressed as either

$$ \mu_i^{\alpha } = \mu_i^{\beta } $$
(1.1)

or

$$ f_i^{\alpha } = f_i^{\beta } $$
(1.1)

.

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© 1987 Springer-Verlag Berlin Heidelberg

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Ganguly, J., Saxena, S.K. (1987). Thermodynamic Functions of Solutions. In: Mixtures and Mineral Reactions. Minerals and Rocks, vol 19. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-46601-4_1

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  • DOI: https://doi.org/10.1007/978-3-642-46601-4_1

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-642-46603-8

  • Online ISBN: 978-3-642-46601-4

  • eBook Packages: Springer Book Archive

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