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Phys. Rev. Lett. 97, 215504 (2006) [4 pages]

Quasihydrostatic Equation of State of Iron above 2 Mbar

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Agnès Dewaele1, Paul Loubeyre1, Florent Occelli1, Mohamed Mezouar2, Peter I. Dorogokupets3, and Marc Torrent1
1DIF/Département de Physique Théorique et Appliquée, CEA, BP 12, 91680 Bruyères-le-Châtel, France
2European Synchrotron Radiation Facility, BP 220, F-38043 Grenoble Cedex, France
3Institute of the Earth’s Crust SB RAS, Irkutsk 664033, Russia

Received 26 July 2006; published 22 November 2006

The compression curve of iron is measured up to 205 GPa at 298 K, under quasihydrostatic conditions in a diamond anvil cell. Above 150 GPa, the compression of this metal is significantly higher than previously measured under nonhydrostatic conditions. The same compression curve is also calculated ab initio and the deviation between experiment and theory is clearly established. A formulation of the equation of state of iron over a large pressure and temperature range, based on the current data and existing shock-wave data, is also proposed. Implications for the Earth’s core are discussed.

© 2006 The American Physical Society

URL:
http://link.aps.org/doi/10.1103/PhysRevLett.97.215504
DOI:
10.1103/PhysRevLett.97.215504
PACS:
62.50.+p, 07.35.+k, 64.30.+t