An equation of state for more than two phases, with an application to the Earth¿s mantle
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| Format: | Artículo científico |
| Langue: | en |
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Universidad Nacional Autónoma de México
2007
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| author | J. A. M. Robles-Dominguez |
| author_facet | J. A. M. Robles-Dominguez |
| contents | An equation of state for more than two phases, with an application to the Earth¿s mantle J. A. M. Robles-Dominguez J. A. Robles-Gutiérrez C. Lomnitz Ciencias de la Tierra non phases isotherms Equation of state additive energies 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 the vicinity of a critical point, it is found that the equation of state must contain atleast three parameters, including the non-additive three-body potential energy. We show how to obtain the interaction spectraof an equation of state for the earth´s mantle. 2007 artículo científico 0016-7169 https://www.redalyc.org/articulo.oa?id=56846302 en http://www.redalyc.org/revista.oa?id=568 Geofísica Internacional application/pdf Universidad Nacional Autónoma de México Geofísica Internacional (México) Num.3 Vol.46 |
| format | Artículo científico |
| id | redalyc_56846302 |
| institution | Redalyc |
| language | en |
| publishDate | 2007 |
| publisher | Universidad Nacional Autónoma de México |
| spellingShingle | An equation of state for more than two phases, with an application to the Earth¿s mantle J. A. M. Robles-Dominguez Ciencias de la Tierra non phases isotherms Equation of state additive energies An equation of state for more than two phases, with an application to the Earth¿s mantle J. A. M. Robles-Dominguez J. A. Robles-Gutiérrez C. Lomnitz Ciencias de la Tierra non phases isotherms Equation of state additive energies 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 the vicinity of a critical point, it is found that the equation of state must contain atleast three parameters, including the non-additive three-body potential energy. We show how to obtain the interaction spectraof an equation of state for the earth´s mantle. 2007 artículo científico 0016-7169 https://www.redalyc.org/articulo.oa?id=56846302 en http://www.redalyc.org/revista.oa?id=568 Geofísica Internacional application/pdf Universidad Nacional Autónoma de México Geofísica Internacional (México) Num.3 Vol.46 |
| title | An equation of state for more than two phases, with an application to the Earth¿s mantle |
| topic | Ciencias de la Tierra non phases isotherms Equation of state additive energies |
| url | https://www.redalyc.org/articulo.oa?id=56846302 |