On the thermodynamics of open systems in geology
β 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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β¦ 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 EarthβAtmosphere, 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.
π SIMILAR VOLUMES
The temperature dependences of the total vapour pressure for solid and liquid InI 2 and liquid InI 3 were measured by the static method with a membran-gauge manometer. The heat capacities above phases and solid InI 3 were also obtained. The partial pressures In 2 I 6 , InI 3 , InI, In 2 I 4 , I 2 ,
The experimental two-component phase diagram between the orientationally disordered crystals 2-amino-2-methyl-1,3-propanediol (AMP) and 1,1,1-tris(hydroxymethyl)propane (PG) has been established from room temperature to the liquid state using thermal analysis and X-ray powder diffraction techniques.