An equation of state for more than two phases, with an application to the Earth¿s mantle
A general equation of state for fl uids of any number of phases is derived. The equation contains the principal experimentalstate equations as special cases. The non-additive energies of 3, 4, particles must also be considered, plus the additive binaryenergies. In order to derive the isotherm in t...
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| Vydáno v: | Geofísica Internacional |
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| Hlavní autoři: | , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Universidad Nacional Autónoma de México
2007
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| Témata: | |
| On-line přístup: | https://www.redalyc.org/articulo.oa?id=56846302 |
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