Abstract
We consider orthoferrite and orthochromite perovskites with the formula , where is a lanthanide and is Fe or Cr. We identify an atomistic interaction that couples the magnetic moments of the and cations with the oxygen octahedral rotations characterizing these crystals. We show that this interaction results in an effective magnetic field acting on the atoms, which in turn explains several intriguing features of these compounds, such as the existence (or absence) of a net magnetization associated with the sublattice and its crystallographic direction. Further, considered together with the couplings described by L. Bellaiche et al. [J. Phys.: Condens. Matter 24, 312201 (2012)], this interaction explains why some compounds display a compensation temperature at which the magnetization cancels and changes sign, while others do not.
- Received 3 September 2015
- Revised 3 November 2015
DOI:https://doi.org/10.1103/PhysRevB.93.014417
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