The magnetic structure and spin-flop transition in the A-site columnar-ordered quadruple perovskite
arXiv:1901.06874 · doi:10.1103/PhysRevB.99.104424
Abstract
We present the magnetic structure of , solved via neutron powder diffraction - the first such study of any A-site columnar-ordered quadruple perovskite to be reported. We demonstrate that long range magnetic order develops below 74 K, and at 28 K a spin-flop transition occurs driven by - exchange and rare earth single ion anisotropy. In both magnetic phases the magnetic structure may be described as a collinear ferrimagnet, contrary to conventional theories of magnetic order in the manganite perovskites. Instead, we show that these magnetic structures can be understood to arise due to ferro-orbital order, the A, A and A site point symmetry, , and the dominance of A-B exchange over both A-A and B-B exchange, which together are unique to the perovskites.
arXiv comment11 pages, 5 figures
References in corpus (6)
- Giant improper ferroelectricity in the ferroaxial magnet CaMn7O12
- Evidence for large electric polarization from collinear magnetism in TmMnO3
- Synthesis and characterization of multiferroic BiMnO
- Modulated spin helicity stabilized by incommensurate orbital density waves in a quadruple perovskite manganite
- Universal magneto-orbital ordering in the divalent -site quadruple perovskite manganites MnO ( = Ca, Sr, Cd, and Pb)
- Evolution of magneto-orbital order upon B-site electron doping in Na1-xCaxMn7O12 quadruple perovskite manganites