Controlling magnetism and transport at perovskite cobaltite interfaces via strain-tuned oxygen vacancy ordering

Shameek Bose, Manish Sharma, Maria A. Torija, Jeff Walter, Nileena Nandakumaran, John Dewey, Josh Schmitt, Jaume Gazquez, Maria Varela, M. Zhernenkov, Michael R. Fitzsimmons, Haile Ambaye, Valeria Lauter, Ondrej Hovorka, Andreas Berger, Chris Leighton

Research output: Contribution to journalArticlepeer-review

Abstract

Complex oxides such as perovskite cobaltites exhibit rich phenomena at interfaces due to the complex interplay between their structural, defect, electronic, and magnetic degrees of freedom. We study this interplay here in the ferromagnetic metallic cobaltite La1-xSrxCoO3-δ, using specific substrates to vary both the heteroepitaxial strain (compressive vs tensile) and growth orientation ((001) vs (110)). Transmission electron microscopy, electron energy-loss spectroscopy, high-resolution X-ray diffraction, magnetometry, polarized neutron reflectometry, and electronic magnetotransport measurements are applied. Lattice mismatch and growth orientation are found to enable the precise control of interfacial oxygen vacancy ordering in La1-xSrxCoO3-δ, thus dictating strain relaxation and oxygen vacancy depth profiles, in turn controlling thickness-dependent magnetic and electronic properties. In particular, compressive strain and (110) orientations minimize deleterious magnetic/electronic dead layer effects, leading to the optimization of interfacial magnetism and transport. Strain and orientation tuning of oxygen vacancy ordering are thus established as powerful means to control physical properties at cobaltite-based interfaces, relevant to several fields.

Original languageEnglish (US)
Article numberL031402
JournalPhysical Review Materials
Volume9
Issue number3
DOIs
StatePublished - Mar 2025

Bibliographical note

Publisher Copyright:
© 2025 American Physical Society.

MRSEC Support

  • Shared

Fingerprint

Dive into the research topics of 'Controlling magnetism and transport at perovskite cobaltite interfaces via strain-tuned oxygen vacancy ordering'. Together they form a unique fingerprint.

Cite this