Coexisting magnetic structures and spin-reorientation in ErDyFeO: Bulk magnetization, neutron scattering, specific heat, and \emph{Ab-initio} studies
arXiv:2108.09975 · doi:10.1103/PhysRevB.105.214436
Abstract
The complex magnetic structures, spin-reorientation and associated exchange interactions have been investigate in ErDyFeO using bulk magnetization, neutron diffraction, specific heat measurements and density functional theory calculations. The Fe spins order as G-type antiferromagnet structure depicted by (,,) irreducible representation below 700K, similar to its end compounds. The bulk magnetization data indicate occurrence of the spin-reorientation and rare-earth magnetic ordering below 75 K and 10 K, respectively. The neutron diffraction studies confirm an "incomplete" (,,) spin-reorientation initiated 75 K. Although, the relative volume fraction of the two magnetic structures varies with decreasing temperature, both co-exist even at 1.5 K. At 8 K, Er/Dy moments order as arrangement develop, which gradually increases in intensity with decreasing temperature. At 2 K, magnetic structure associated with arrangement of Er/Dy moments also appears. At 1.5 K the magnetic structure of Fe spins is represented by a combination of ++, while the rare earth moments coexists as and corresponding to and representation, respectively. The observed Schottky anomaly at 2.5 K suggests that the "rare-earth ordering" is induced by polarization due to Fe spins. The Er-Fe and Er-Dy exchange interactions, obtained from first principle calculations, primarily cause the complicated spin-reorientation and rare-earth ordering, respectively, while the dipolar interactions between rare-earth moments, result in the type rare-earth ordering at 2 K.
15 pages, 11 figures
References in corpus (4)
- Ground state and magnetic phase transitions of orthoferrite DyFeO_3
- Interplay of 4f-3d Magnetism and Ferroelectricity in DyFeO3
- Magnetic ground state of the Ising-like antiferromagnet DyScO
- Magnetic order of Dy and Fe moments in antiferromagnetic DyFeO probed by spin Hall magnetoresistance and spin Seebeck effect