Site-specific magnetization reversal studies of magnetite

A. Cady, D. Haskel, J. C. Lang, Z. Islam, G. Srajer, A. Ankudinov, G. Subìas, and J. Garcìa
Phys. Rev. B 73, 144416 – Published 14 April 2006

Abstract

The mechanism of magnetization reversal in magnetite (Fe3O4) single crystals was studied using site-specific magnetic sensitive diffraction anomalous near-edge structure. By exploiting the angular dependence of the cross section, we are able to show that the mechanism of reversal involves a mixture of coherent rotation and domain formation. The results reveal additional details to that provided by XMCD measurements, which average over nonequivalent sites.

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  • Received 7 November 2005
  • Corrected 20 April 2006

DOI:https://doi.org/10.1103/PhysRevB.73.144416

©2006 American Physical Society

Corrections

20 April 2006

Erratum

Publisher's Note: Site-specific magnetization reversal studies of magnetite [Phys. Rev. B 73, 144416 (2006)]

A. Cady, D. Haskel, J. C. Lang, Z. Islam, G. Srajer, A. Ankudinov, G. Subìas, and J. Garcìa
Phys. Rev. B 73, 149906 (2006)

Authors & Affiliations

A. Cady1, D. Haskel1, J. C. Lang1, Z. Islam1, G. Srajer1, A. Ankudinov2, G. Subìas3, and J. Garcìa3

  • 1Advanced Photon Source, Argonne National Laboratory, Argonne, Illinois 60439, USA
  • 2Department of Physics, University of Washington, Seattle, Washington 98195, USA
  • 3Instituto de Ciencia de Materiales de Aragón, CSIC-Universidad de Zaragoza, Pza. San Francisco s/n 50009 Zaragoza, Spain

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Issue

Vol. 73, Iss. 14 — 1 April 2006

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