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Giant anisotropy of magnetic damping in an epitaxial Cr/Fe bilayer with the absence of magnetocrystalline anisotropy

Thanh-Huong Thi Nguyen1, Jungmin Park2, Jae-Hyun Ha1, Soogil Lee3, Van Quang Nguyen4, Nyun Jong Lee5, Byong-Guk Park3, Sunglae Cho5, Jung-Il Hong1,* et al.

Sanghoon Kim5,†

  • 1Department of Physics and Chemistry, Daegu Gyeongbuk Institute of Science and Technology, Daegu 42988, Korea
  • 2Department of Physics, Korea Advanced Institute of Science and Technology, Daejeon 34141, Korea
  • 3Department of Materials Science and Engineering, Korea Advanced Institute of Science and Technology, Daejeon 34141, Korea
  • 4Korea Atomic Energy Research Institute, Daejeon 34057, Korea
  • 5Department of Physics, University of Ulsan, Ulsan 44610, Korea

  • *Corresponding author: jihong@dgist.ac.kr
  • †Corresponding author: sanghoon.kim@ulsan.ac.kr

Phys. Rev. Materials 8, L041401 – Published 1 April, 2024

DOI: https://doi.org/10.1103/PhysRevMaterials.8.L041401

Abstract

Magnetic damping is one of the most important parameters governing the critical current density for current-induced magnetization switching in spin-torque devices. The anisotropic nature of magnetic damping, influenced by both intrinsic and extrinsic factors, has been demonstrated in both theoretical and experimental studies. Nevertheless, understanding the underlying mechanisms of magnetic damping anisotropy, particularly in the bilayer structure of a ferromagnet and a nonmagnetic metal, remains an open challenge. In this study, we investigate the crystallographic dependence of magnetic damping in an epitaxial Cr/Fe bilayer, which has negligible magnetocrystalline anisotropy. We experimentally extracted the total damping by conducting frequency-dependent ferromagnetic resonance measurement at different in-plane angles. The observed damping reveals a strong angular dependence with an anisotropy of ∼400% in the bilayer. All possible contributions to the total damping will be discussed carefully to clarify the origin of the profound damping anisotropy observed in our Cr/Fe bilayer.

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