Martensitic fcc-hcp transformation pathway in solid krypton and xenon and its effect on their equations of state

A. D. Rosa, A. Dewaele, G. Garbarino, V. Svitlyk, G. Morard, F. De Angelis, M. Krstulović, R. Briggs, T. Irifune, O. Mathon, and M. A. Bouhifd
Phys. Rev. B 105, 144103 – Published 15 April 2022
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Abstract

The martensitic transformation is a fundamental physical phenomenon at the origin of important industrial applications. However, the underlying microscopic mechanism, which is of critical importance to explain the outstanding mechanical properties of martensitic materials, is still not fully understood. This is because for most martensitic materials the transformation is a fast process that makes in situ studies extremely challenging. Noble solids krypton and xenon undergo a progressive pressure-induced face-centered cubic (fcc) to hexagonal close-packed (hcp) martensitic transition with a very wide coexistence domain. Here, we took advantage of this unique feature to study the detailed transformation progress at the atomic level by employing in situ x-ray diffraction and absorption spectroscopy. We evidenced a four-stage pathway and suggest that the lattice mismatch between the fcc and hcp forms plays a key role in the generation of strain. We also determined precisely the effect of the transformation on the compression behavior of these materials.

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  • Received 20 December 2021
  • Revised 8 March 2022
  • Accepted 17 March 2022

DOI:https://doi.org/10.1103/PhysRevB.105.144103

©2022 American Physical Society

Physics Subject Headings (PhySH)

Condensed Matter, Materials & Applied Physics

Authors & Affiliations

A. D. Rosa1,*, A. Dewaele2,3, G. Garbarino1, V. Svitlyk1, G. Morard4, F. De Angelis5, M. Krstulović6, R. Briggs7, T. Irifune8, O. Mathon1, and M. A. Bouhifd9

  • 1European Synchrotron Radiation Facility (ESRF), 71, Avenue des Martyrs, Grenoble, France
  • 2CEA, DAM, DIF, 91297 Arpajon Cedex, France
  • 3Université Paris-Saclay, CEA, Laboratoire Matière en Conditions Extrêmes, 91680 Bruyères-le-Châtel, France
  • 4Université Grenoble Alpes, Université Savoie Mont Blanc, CNRS, IRD, IFSTTAR, ISTerre, 38000 Grenoble, France
  • 5Dipartimento di Fisica, Universita' di Roma La Sapienza - Piazzale Aldo Moro 5, 00185 Roma, Italy
  • 6University of Potsdam, Institute of Geosciences, Karl-Liebknecht-Str. 24–25, 14476 Potsdam-Golm, Germany
  • 7Lawrence Livermore National Laboratory, Livermore, California 94500, USA
  • 8Geodynamics Research Center, Ehime University, 2–5 Bunkyo-cho, Matsuyama 790–8577, Japan
  • 9Laboratoire Magmas et Volcans, Université Clermont Auvergne, CNRS, IRD, OPGC, F-63000 Clermont-Ferrand, France

  • *angelika.rosa@esrf.fr

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Issue

Vol. 105, Iss. 14 — 1 April 2022

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