Mechanism of the αε phase transformation in iron

A. Dewaele, C. Denoual, S. Anzellini, F. Occelli, M. Mezouar, P. Cordier, S. Merkel, M. Véron, and E. Rausch
Phys. Rev. B 91, 174105 – Published 14 May 2015

Abstract

The α-Feε-Fe pressure-induced transformation under pure hydrostatic static compression has been characterized with in situ x-ray diffraction using α-Fe single crystals as starting samples. The forward transition starts at 14.9 GPa, and the reverse at 12 GPa, with a width of αε coexistence domain of the order of 2 GPa. The elastic stress in the sample increases in this domain, and partially relaxes after completion of the transformation. Orientation relations between parent α-Fe and child ε-Fe have been determined, which definitely validates the Burgers path for the direct transition. On the reverse transition, an unexpected variant selection is observed. X-ray diffraction data, complemented with ex situ microstructural observations, suggest that this selection is caused by defects and stresses accumulated during the direct transition.

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  • Received 23 June 2014
  • Revised 10 March 2015

DOI:https://doi.org/10.1103/PhysRevB.91.174105

©2015 American Physical Society

Authors & Affiliations

A. Dewaele1, C. Denoual1, S. Anzellini1, F. Occelli1, M. Mezouar2, P. Cordier3, S. Merkel3, M. Véron4, and E. Rausch4

  • 1Commissariat à l'Energie Atomique, Direction des Applications Militaires, Ile de France, F-91297 Arpajon, France
  • 2European Synchrotron Radiation Facility, BP220, 38043 Grenoble Cedex, France
  • 3Unité Matériaux et Transformations, Université Lille 1, UMR CNRS 8207, F-59655 Villeneuve d'Ascq Cedex, France
  • 4Laboratoire SIMaP, Grenoble INP-CNRS-UJF, BP 75, 38402 Saint Martin d'Hères Cedex, France

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Vol. 91, Iss. 17 — 1 May 2015

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