Ferrimagnetism in the double perovskite Ca2FeOsO6: a density functional study
arXiv:1406.3101 · doi:10.1103/PhysRevB.90.054406
Abstract
Using density functional calculations, we find that the newly synthesized CaFeOsO has the high-spin Fe ()-Os () state. The octahedral Os ion has a large intrinsic exchange splitting, and its configuration makes the spin-orbit coupling ineffective. Moreover, there is a strong antiferromagnetic (AF) coupling between the neighboring Fe ( = 5/2) and Os ( = -3/2), but the AF couplings within both the fcc Fe and Os sublattices are one order of magnitude weaker. Therefore, a magnetic frustration is suppressed and a stable ferrimagnetic (FiM) ground state appears. This FiM order is due to the virtual hopping of the electrons from Os () to Fe (). However, if the experimental bended Fe-O-Os exchange path gets straight, the hopping from Fe () to Os () would be facilitated and then a ferromagnetic (FM) coupling would occur.
arXiv comment5 pages, 5 figures
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- Long-range magnetic interaction and frustration in double perovskite SrNiIrO
- Understanding the Magnetic Puzzles of Double Perovskites A2FeOsO6 (A=Ca, Sr)
- The role of nonmagnetic d0 vs. d10 B-type cations on the magnetic exchange interactions in osmium double perovskites
- Room-temperature ferrimagnetism of anti-site-disordered Ca2MnOsO6
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- New Buckled Honeycomb Lattice Compound Sr3CaOs2O9 Exhibiting Antiferromagnetism above Room Temperature
- Re-t2g-splitting-driven semiconductor gaps in ferrimagnetic double perovskite Ca2MReO6 (M=Cr,Fe) from first principles
- Magnetic frustration in the cubic double perovskite Ba2NiIrO6
- Spin-Orbital States and Strong Antiferromagnetism of Layered EuSrFeO and SrFeOCl