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Neutron diffraction evidence for the spin-reorientational transition in FeBO3 at high pressures

  • Condensed Matter
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Abstract

The spin-reorientational transition from the state with “easy-plane” anisotropy to the state with “easy-axis” anisotropy—a pressure analogue of the Morin temperature transition in hematite— was detected in iron borate at a pressure of P∼17 kbar at room temperature by the neutron diffraction method.

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Authors and Affiliations

  1. Russian Research Centre Kurchatov Institute, pl. Kurchatova 1, Moscow, 123182, Russia

    V. P. Glazkov, V. V. Kvardakov & V. A. Somenkov

Authors
  1. V. P. Glazkov
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  2. V. V. Kvardakov
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  3. V. A. Somenkov
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Additional information

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Translated from Pis’ma v Zhurnal Éksperimental’no\(\overset{\lower0.5em\hbox{$\smash{\scriptscriptstyle\smile}$}}{l} \) i Teoretichesko\(\overset{\lower0.5em\hbox{$\smash{\scriptscriptstyle\smile}$}}{l} \) Fiziki, Vol. 71, No. 4, 2000, pp. 238–240.

Original Russian Text Copyright © 2000 by Glazkov, Kvardakov, Somenkov.

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Glazkov, V.P., Kvardakov, V.V. & Somenkov, V.A. Neutron diffraction evidence for the spin-reorientational transition in FeBO3 at high pressures. Jetp Lett. 71, 165–166 (2000). https://doi.org/10.1134/1.568305

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  • DOI: https://doi.org/10.1134/1.568305

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