Minerals and Solids at High Temperature and High Pressure: Equations of State and Thermodynamics
A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Crystallography and Physical Chemistry of Minerals & Nanominerals".
Deadline for manuscript submissions: closed (13 November 2020) | Viewed by 4608
Special Issue Editors
Interests: equation of state; high pressure high temperature experiments; mineral physics at extreme conditions; elasticity; compressibility; PVT properties; ab initio calculation; phase diagrams
Interests: mantle; high pressures and temperatures; xenoliths; phase transitions; equations of state; oxidation state; experiments
Special Issues, Collections and Topics in MDPI journals
Special Issue Information
Dear Colleagues,
Mineral physics studies provide key knowledge on thermodynamic properties of constituents of the Earth’s and planetary interiors. Equations of state (EoS) remain a resourceful and powerful tool to model and evaluate the thermodynamic behaviors of any physical–chemical system. EoS characterizes the state of matter of a material under a given set of physical conditions and may be used to describe gases, fluids, fluid mixtures, and solids. In mineral physics, an EoS is used to determine how the volume (or density) of a material vary as a function of pressure and temperature. It reflects the atomic structure, chemical bonding, and stability of a material. This information, combined with geophysical and geochemical observations, helps to constrain the structure and dynamics of the Earth and other planets.
This Special Issue aims to include a representative group of experimental and theoretical papers in the field of equations of state and thermodynamic properties of minerals (as well as melts, fluids, and rocks) at high pressures and temperatures.
Dr. Peter I. Dorogokupets
Dr. Anna M. Dymshits
Guest Editors
Manuscript Submission Information
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Keywords
- equation of state
- high pressure high temperature experiments
- mineral physics at extreme conditions
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