articleJournal of Metamorphic GeologyFeb 16, 2011Closed access

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

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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…

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Authors

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Topics & keywords

Keywords
  • Thermodynamics
  • Thermal expansion
  • Compressibility
  • Equation of state
  • Bulk modulus
  • Silicate
  • Mantle (geology)
  • Thermodynamic equilibrium
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