Computational searches for iron carbide in the Earth's inner core

Gihan L. Weerasinghe, R. J. Needs, and Chris J. Pickard
Phys. Rev. B 84, 174110 – Published 21 November 2011
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Abstract

We have used density-functional-theory methods together with a structure searching algorithm to determine stable structures and stoichiometries of mixtures of iron and carbon at high pressures and zero temperature. The most favorable stoichiometries at Earth's inner-core pressures (350 GPa) are those with between about 20% and 35% carbon atoms. The most stable stoichiometries were found to be (Fe and C), Fe3C, Fe7C3, and Fe2C. The latter has not to our knowledge been discussed previously in relation to the Earth's core. The stoichiometries Fe4C and Fe5C2 were found to be close to stability at Earth's inner-core pressures. We find that Fe7C3 is unstable to decomposition into Fe3C + 2Fe2C at pressures greater than 330 GPa. At 150 GPa only Fe, C, Fe3C, and Fe7C3 are stable. Formation of Fe/C compounds is energetically more favorable at 350 GPa than at 150 GPa. We also report a new phase for Fe3C with Cmcm symmetry to be more stable than the well-known cementite phase at 350 GPa. A number of pressure-induced phase transitions are identified in Fe3C, Fe3C2, FeC, Fe8C, and FeC2. The lowest enthalpy Fe/C phases were found to be metallic at the pressures studied.

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  • Received 15 June 2011

DOI:https://doi.org/10.1103/PhysRevB.84.174110

©2011 American Physical Society

Authors & Affiliations

Gihan L. Weerasinghe and R. J. Needs

  • Theory of Condensed Matter Group, Cavendish Laboratory, J J Thomson Avenue, Cambridge CB3 0HE, United Kingdom

Chris J. Pickard

  • Department of Physics and Astronomy, University College London, Gower Street, London WC1E 6BT, United Kingdom

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Issue

Vol. 84, Iss. 17 — 1 November 2011

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