Magnetic Instabilities in Fe3C Cementite Particles Observed with Fe K-Edge X-Ray Circular Dichroism under Pressure

E. Duman, M. Acet, E. F. Wassermann, J. P. Itié, F. Baudelet, O. Mathon, and S. Pascarelli
Phys. Rev. Lett. 94, 075502 – Published 23 February 2005

Abstract

The ferromagnetic interstitial iron compound Fe3C (cementite) is expected to have Invar properties, whereby a high-moment to low-moment transition should occur when the atomic volume is reduced below a critical value. We, therefore, examine the pressure dependence of the Fe K-edge x-ray magnetic circular dichroism in Fe3C at ambient temperature and pressures up to 20 GPa. We find clear evidence for a high-moment to low-moment transition around 10 GPa.

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  • Received 1 October 2004

DOI:https://doi.org/10.1103/PhysRevLett.94.075502

©2005 American Physical Society

Authors & Affiliations

E. Duman, M. Acet*, and E. F. Wassermann

  • Experimentalphysik, Universität Duisburg-Essen, D-47048 Duisburg, Germany

J. P. Itié

  • Physique des Milieux Condensés, CNRS-UMR 7602, Université Paris VI, B77 4, place Jussieu, F-75252 Paris CEDEX 05, France

F. Baudelet

  • Syncrotron Soleil L'Orme des Merisiers, Saint-Aubin-BP 48 F-91192 Gif-sur-Yvette Cedex, France

O. Mathon and S. Pascarelli

  • European Synchrotron Radiation Facility, B.P. 220, F-38043 Grenoble Cedex, France

  • *Corresponding author. Electronic address: macet@ttphysik.uni-duisburg.de

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Issue

Vol. 94, Iss. 7 — 25 February 2005

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