Simple Realistic Model of Spin Reorientation in 4f-3d Compounds
Abstrak
This is a simple but realistic microscopic theory of spontaneous spin reorientation in rare-earth perovskites, orthoferrites <i>R</i>FeO<inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><msub><mrow></mrow><mn>3</mn></msub></semantics></math></inline-formula> and orthochromites <i>R</i>CrO<inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><msub><mrow></mrow><mn>3</mn></msub></semantics></math></inline-formula>, induced by the 4f-3d interaction, namely, the interaction of the well-isolated ground-state Kramers doublet or non-Kramers quasi-doublet of the 4f ion with an effective magnetic field induced by 3d sublattice. Both the temperature and the nature of the spin-reorientation transition are the result of competition between the second- and fourth-order spin anisotropy of the 3d sublattice, the crystal field for 4f ions, and 4f-3d interaction.
Topik & Kata Kunci
Penulis (3)
Alexander Moskvin
Evgenii Vasinovich
Anton Shadrin
Akses Cepat
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- 2022
- Sumber Database
- DOAJ
- DOI
- 10.3390/magnetochemistry8040045
- Akses
- Open Access ✓