Quantification of residual stress governing the spin-reorientation transition (SRT) in amorphous magnetic thin films

  • Darragh Cronin
  • , M. Hardiman
  • , D. Lordan
  • , G. Wei
  • , P. McCloskey
  • , C. Oʹ Mathúna
  • , A. Masood

Research output: Contribution to journalArticlepeer-review

Abstract

Soft magnetic thin films with in-plane uniaxial magnetic anisotropy are of significant importance for a broad range of technological applications, including high-frequency power conversion. In-plane uniaxial anisotropy in amorphous films is of particular interest for ultra-low materials loss and MHz frequency operations. The present work is focused on one of the fundamental mechanisms, i.e., residual stress, that can negate the uniaxial anisotropy in amorphous films by engendering perpendicular magnetisation and hence, undermining the soft magnetic performance. It is quantified how the nature of residual stress, compressive or tensile, transforms the magnetisation from an in-plane to an out-of-plane configuration, also well-known as spin-reorientation transition (SRT). A correlation between engineered residual stress in multilayer stacks, induced by the uneven expansion of metallic/dielectric layers following a thermal-shock scheme, and SRT mechanism demonstrates tensile stress inside the films undermines the soft magnetic performance. We suggest the magnetic softness can be retained by eluding sources of tensile stress during fabrication or post-processing of the amorphous films.

Original languageEnglish
Article number167572
JournalJournal of Magnetism and Magnetic Materials
Volume522
DOIs
Publication statusPublished - 15 Mar 2021

Keywords

  • Magnetoelastic anisotropy
  • Multilayer stacks
  • Nano-indentation
  • Perpendicular magnetisation
  • Residual stress
  • Spin-reorientation transition

Fingerprint

Dive into the research topics of 'Quantification of residual stress governing the spin-reorientation transition (SRT) in amorphous magnetic thin films'. Together they form a unique fingerprint.

Cite this