## 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 eq
Note on the use of the Krupkowski relation in the thermodynamic study of AIII—BV systems
✍ Scribed by Dr.-Ing. V. Flemr; Prof. Dr. B. Hájek
- Publisher
- John Wiley and Sons
- Year
- 1983
- Tongue
- English
- Weight
- 80 KB
- Volume
- 18
- Category
- Article
- ISSN
- 0232-1300
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A simple, general expression is derived which permits the calculation of AFa -AF" from the phase diagrams for binary systems with complete solid solubility. In systems with a narrow liquidus-solidus gap good values of A(AF) may be obtained without any use of detailed information on the free energy
dedicated to professor leonard gross on the occasion of his 70th birthday Functions of bounded variation (BV functions) are defined on an abstract Wiener space (E, H, +) in a way similar to that in finite dimensions. Some characterizations are given, which justify describing a BV function as a funct