Deformation and slip systems of CaCl2-type MnO2 under high pressure

Binbin Yue, Matthias Krug, Carmen Sanchez-Valle, Sébastien Merkel, and Fang Hong
Phys. Rev. Materials 6, 053603 – Published 3 May 2022

Abstract

Many nonmetals and metal dioxides MO2, including the dense form of SiO2 stishovite, crystalize in a rutile structure at low pressure and transform to a denser CaCl2 structure under high pressure. Structures and transformations in MO2 dioxides hence serve as an archetype for applications in materials science and inside the Earth and terrestrial planets. Despite its significance, however, the deformation behavior of MO2 compounds in the CaCl2 structure is very poorly constrained. Here we use radial x-ray diffraction in a diamond-anvil cell and study MnO2 as a representative system of the MO2 family. We identify the dominant slip systems and constrain texture evolution in CaCl2-structured phases. After phase transition to a CaCl2 structure above 3.5 GPa, the dominant (010)[100] and secondary {110}[001] and {011}[0-11] slip systems induce a 121 texture in compression. Further compression increases the activity of the {011}011 slip system, with an enhanced 001 texture at 50GPa. During pressure release, the 001 texture becomes dominant over the original 121 texture. This clearly demonstrates the effect of pressure on the deformation behavior and slip systems of CaCl2-structured dioxides. Finally, MnO2 transforms back to a rutile structure upon pressure release, with a significant orientation memory, highlighting the martensitic nature of the CaCl2 to rutile structural transformation. These findings provide key guidance regarding the plasticity of CaCl2-structured dioxides, with implications in materials and Earth and planetary science.

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  • Received 14 December 2021
  • Accepted 15 April 2022

DOI:https://doi.org/10.1103/PhysRevMaterials.6.053603

©2022 American Physical Society

Physics Subject Headings (PhySH)

Condensed Matter, Materials & Applied Physics

Authors & Affiliations

Binbin Yue1,*, Matthias Krug2, Carmen Sanchez-Valle2, Sébastien Merkel3,†, and Fang Hong4,5,6,‡

  • 1Center for High Pressure Science & Technology Advanced Research, 10 East Xibeiwang Road, Haidian, Beijing 100094, China
  • 2Institute for Mineralogy, University of Münster, 48149 Münster, Germany
  • 3Univ. Lille, CNRS, INRAE, Centrale Lille, UMR 8207 - UMET - Unité Matériaux et Transformations, F-59000 Lille, France
  • 4Beijing National Laboratory for Condensed Matter Physics, Institute of Physics, Chinese Academy of Sciences, Beijing 100190, China
  • 5School of Physical Sciences, University of Chinese Academy of Sciences, Beijing 100190, China
  • 6Songshan Lake Materials Laboratory, Dongguan, Guangdong 523808, China

  • *yuebb@hpstar.ac.cn
  • sebastien.merkel@univ-lille.fr
  • hongfang@iphy.ac.cn

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Vol. 6, Iss. 5 — May 2022

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