FeRh ground state and martensitic transformation

Nikolai A. Zarkevich and Duane D. Johnson
Phys. Rev. B 97, 014202 – Published 9 January 2018

Abstract

Cubic B2 FeRh exhibits a metamagnetic transition [(111) antiferromagnet (AFM) to ferromagnet (FM)] around 353 K and remains structurally stable at higher temperatures. However, the calculated zero-Kelvin phonons of AFM FeRh exhibit imaginary modes at M points in the Brillouin zone, indicating a premartensitic instability, which is a precursor to a martensitic transformation at low temperatures. Combining electronic-structure calculations with ab initio molecular dynamics, conjugate gradient relaxation, and the solid-state nudged-elastic band methods, we predict that AFM B2 FeRh becomes unstable at ambient pressure and transforms without a barrier to an AFM(111) orthorhombic (martensitic) ground state below 90±10K. We also consider competing structures, in particular, a tetragonal AFM(100) phase that is not the global ground state, as proposed [Phys. Rev. B 94, 180407(R) (2016)], but a constrained solution.

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  • Received 11 October 2017
  • Revised 25 November 2017

DOI:https://doi.org/10.1103/PhysRevB.97.014202

©2018 American Physical Society

Physics Subject Headings (PhySH)

Condensed Matter, Materials & Applied Physics

Authors & Affiliations

Nikolai A. Zarkevich1,* and Duane D. Johnson1,2,†

  • 1Ames Laboratory, U.S. Department of Energy, Iowa State University, Ames, Iowa 50011-3020, USA
  • 2Department of Materials Science & Engineering, Iowa State University, Ames, Iowa 50011, USA

  • *zarkev@ameslab.gov
  • ddj@iastate.edu, ddj@ameslab.gov

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Issue

Vol. 97, Iss. 1 — 1 January 2018

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