Large room-temperature spin-dependent tunneling magnetoresistance in polycrystalline Fe3O4 films
- 20 October 2003
- journal article
- research article
- Published by AIP Publishing in Applied Physics Letters
- Vol. 83 (17), 3531-3533
- https://doi.org/10.1063/1.1622440
Abstract
Polycrystalline films have been prepared by reactive sputtering at room temperature. Transmission electron microscopy images show that the films consist of quite uniform grains well separated by grain boundaries. It was found that the tunneling of spin-polarized electrons across the antiferromagnetic coupled grain boundaries dominates the transport properties of the films. Magnetoresistance (MR) shows linear and quadratic magnetic-field dependence in the low-field range when the field is applied parallel and perpendicular to film plane, which is similar to the behaviors observed in the epitaxial films consisting of a large fraction of antiferromagnetic antiphase domain boundaries. At 300 K, the size of the MR reaches −7.4% under a 50-kOe magnetic field, which is a very large MR for polycrystalline films.
Keywords
This publication has 20 references indexed in Scilit:
- Spin-Polarized Transport across Sharp Antiferromagnetic BoundariesPhysical Review Letters, 2002
- Development of half-metallic ultrathin Fe3O4 films for spin-transport devicesApplied Physics Letters, 2002
- Fabrication and properties of heteroepitaxial magnetite (Fe3O4) tunnel junctionsApplied Physics Letters, 1998
- Enhanced Magnetoresistance in Insulating Granular Systems: Evidence for Higher-Order TunnelingPhysical Review Letters, 1998
- Magnetoresistance and magnetic properties of epitaxial magnetite thin filmsPhysical Review B, 1997
- Theory of tunneling magnetoresistance in granular magnetic filmsPhysical Review B, 1996
- Electron states, magnetism, and the Verwey transition in magnetitePhysical Review B, 1991
- Band Structure in the High Temperature Phase of Fe3O4Journal of the Physics Society Japan, 1984
- New Class of Materials: Half-Metallic FerromagnetsPhysical Review Letters, 1983
- Electronic Conduction of Magnetite (Fe3O4) and its Transition Point at Low TemperaturesNature, 1939