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Updated: Sep 27, 2025

Visualizing Uniaxial-strain Manipulation of Antiferromagnetic Domains in Fe1+YTe Using a Spin-polarized Scanning Tunneling Microscope
Published on: March 24, 2019
The magnetic structure of DyFeO3revisited: Fe spin reorientation and Dy incommensurate magnetic order
Clemens Ritter1, Rui Vilarinho2, Joaquim Agostinho Moreira2
1Institut Laue-Langevin, 71 Avenue des Martyrs, 38042 Grenoble, France.
Abstract:
High resolution and high intensity neutron powder diffraction is used to study the ground state magnetic order and the spin reorientation transition in the orthoferrite DyFeO3. The transition from the high temperaturek= 0 Γ4(GAF) to the low temperature Γ1(AGC) type order of the Fe-sublattice is found atTSR= 73 K and does not show any thermal hysteresis. BelowTN2= 4 K the Dy-sublattice orders in an incommensurate magnetic structure withk= [0, 0, 0.028] while the Fe-sublattice keeps its commensurate Γ1type order. DyFeO3is the first orthoferriteRFeO3to possess an incommensurate magnetic order of the rare earth sublattice under zero field conditions; an important piece of information neglected in the recent discussion of its multiferroic properties.
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