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On the thermodynamics of open systems in geology

✍ Scribed by I. A. Ostrovsky


Publisher
John Wiley and Sons
Year
2007
Tongue
English
Weight
299 KB
Volume
9
Category
Article
ISSN
0072-1050

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✦ Synopsis


Abstract

Semipermeable membranes are necessary conditions for the realisation of equilibrium open systems in the Earth's crust. Membraneless cases, as at the boundary Earth‐Atmosphere, are rather exceptional. The application of the D. S. Korzhinskii's thermodynamics of open systems to mineral equilibria in rocks may be justified only if the perfect mobility of components is proved independently viz: by means other than the analysis of mineral paragenesis alone.


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