4.7 Article

Influence of the Cubic Sublattice on Magnetic Coupling between the Tetrahedral Sites of Garnet

Journal

INORGANIC CHEMISTRY
Volume 60, Issue 12, Pages 8500-8506

Publisher

AMER CHEMICAL SOC
DOI: 10.1021/acs.inorgchem.1c00113

Keywords

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Funding

  1. Office of Naval Research [N00014-15-1-2411]
  2. U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences [DE-AC02-06CH11357]
  3. Leverhulme Trust [RPG-2018-268]

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The study reveals that despite well-pronounced magnetic transitions at low temperatures in both iron-based garnets, there is evidence of diffuse magnetic scattering due to competition within the tetrahedral sites, resulting in a complex noncollinear magnetic structure with a mixture of ferro- and antiferromagnetic interactions.
We present a study on the nuclear and magnetic structures of two iron-based garnets with magnetic cations isolated on tetrahedral sites. Ca2YZr2Fe3O12 and Ca2LaZr2Fe3O12 offer an interesting comparison for examining the effect of increasing cation size within the diamagnetic backbone of the garnet crystal structure, and how such changes affect the magnetic order. Despite both systems exhibiting well-pronounced magnetic transitions at low temperatures, we also find evidence for diffuse magnetic scattering due to a competition between the nearest-neighbor, next nearest-neighbor, and so on, within the tetrahedral sites. This competition results in a complex noncollinear magnetic structure on the tetrahedral sublattice creating a mixture of ferro- and antiferromagnetic interactions above the long-range ordering temperature near 20 K and suggests that the cubic site of the garnet plays a significant role in mediating the superexchange interactions between tetrahedral cations.

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