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Thermodynamic properties at the Earth's core conditions and the shock-reduced isotherm of iron: a first-principles study
KTH, Superseded Departments, Materials Science and Engineering.
2002 (English)In: Journal of Physics: Condensed Matter, ISSN 0953-8984, E-ISSN 1361-648X, Vol. 14, no 31, 7321-7335 p.Article in journal (Refereed) Published
Abstract [en]

First-principles thermodynamic calculations for metal iron (Fe) at ultrahigh pressures and temperatures are reported. The calculated results can be divided into three major parts: (i) the static 300 K equation of state and the dynamic shock-wave Hugoniot at pressures up to 1000 GPa; (ii) the shock-reduced data for the 300 K isotherm; and (iii) the thermodynamic properties under the Earth's core conditions. The calculations are parameter free in the sense that the cold part of the Helmholtz free energy is calculated using the full-potential linearized augmented-plane-wave method within the generalized gradient approximation. The thermal part due to the lattice ions is calculated using the recently developed classical mean-field potential approach, and the thermal part due to the thermal electrons is calculated using the one-dimensional numerical integration technique. The calculated results agree well with the available experimental data.

Place, publisher, year, edition, pages
2002. Vol. 14, no 31, 7321-7335 p.
Keyword [en]
generalized-gradient approximation, static compression, phase-transition, high-pressures, liquid-iron, inner-core, x-ray, equation, wave, gpa
Identifiers
URN: urn:nbn:se:kth:diva-21865ISI: 000177799900006OAI: oai:DiVA.org:kth-21865DiVA: diva2:340563
Note
QC 20100525Available from: 2010-08-10 Created: 2010-08-10 Last updated: 2017-12-12Bibliographically approved

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