The Grüneisen parameter, the melting curve and the adiabatic gradient for mantle and core

Details The Grüneisen parameter, the melting curve and the adiabatic gradient for mantle and core The Grüneisen parameter, the melting curve and the adiabatic gradient for mantle and core

Jun 1980

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1980pepi...22d...4z&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 22, Issue 3-4, p. iv-iv.

Physics

Scientific paper

A knowledge of the Grüneisen parameter is essential for the determination of many basic physical relationships important in the study of the Earth. These include the equation of state for solids and liquids, the adiabatic gradient and the melting curve for the Earth's interior, the thermodynamic properties of the mantle and core, and the Hugoniot curve (the shock wave adiabat). We present theoretical results for the determination of the Grüneisen parameter γ(ρ) and analyse the approximate methods used for its determination. The results of these determinations give γ(ρ) in the pressure range from 0 to 100 Mbar.

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