An improved and extended internally consistent thermodynamic dataset for phases of petrological interest, involving a new equation of state for solids
University of Cambridge · University of Melbourne
Abstract
The thermodynamic properties of 254 end-members, including 210 mineral end-members, 18 silicate liquid end-members and 26 aqueous fluid species are presented in a revised and updated internally consistent thermodynamic data set. The PVT properties of the data set phases are now based on a modified Tait equation of state (EOS) for the solids and the Pitzer & Sterner (1995) equation for gaseous components. Thermal expansion and compressibility are linked within the modified Tait EOS (TEOS) by a thermal pressure formulation using an Einstein temperature to model the temperature dependence of both the thermal expansion and bulk modulus in a consistent way. The new EOS has led to improved fitting of the phase…
Citation impact
- FWCI
- 29.23
- Percentile
- 100%
- References
- 663
Authors
2Topics & keywords
- Thermodynamics
- Thermal expansion
- Compressibility
- Equation of state
- Bulk modulus
- Silicate
- Mantle (geology)
- Thermodynamic equilibrium