Triple A-Site Cation Ordering in the Ferrimagnetic YCuGaMnO Perovskite.

Inorg Chem

International Center for Materials Nanoarchitectonics (WPI-MANA), National Institute for Materials Science (NIMS), Namiki 1-1, Tsukuba, Ibaraki 305-0044, Japan.

Published: September 2022

AI Article Synopsis

  • A high-pressure, high-temperature method was used to prepare a new perovskite compound, YCuGaMnO, which displays a unique triple cation ordering and some anti-site disorder among 3d transition metals in its crystal structure.
  • The compound exhibits long-range ferrimagnetic order at 115 K, with specific magnetic moments aligned along the axis, differing from its "parent" compound YMnGaMnO which exhibits spin-glass properties.
  • Thermal expansion behavior of YCuGaMnO is anisotropic, showing distinct changes in lattice parameters at various temperatures, decreasing at first and then increasing as temperature rises.

Article Abstract

A new member of A-site columnar-ordered AA'A″BO quadruple perovskites with the composition of YCuGaMnO was prepared by a high-pressure, high-temperature method at 6 GPa and about 1500 K. Its crystal structure and cation distributions were studied by powder synchrotron X-ray and neutron diffraction. There is a triple A-site cation ordering with some degrees of anti-site disorder among sites occupied by 3d transition metals: [Y][CuMn][GaMn][MnCuGa]O. It has the space group 4/ (no. 137) between 1.5 and 873 K with = 7.33884 Å and = 7.66251 Å at 297 K. Despite anti-site disorder, it exhibits a long-range ferrimagnetic order at = 115 K with the ordered moment of 2.19 μ at each B site and 0.89 μ at the A' or A″ site. Magnetic moments are aligned along the axis; all moments are ordered ferromagnetically at the B sites, and the moments at the A' or A″ site are ordered in the opposite direction. Cu doping drastically changes magnetic properties as "parent" YMnGaMnO just shows spin-glass magnetic properties without long-range ordering. Anisotropic thermal expansion was observed in YCuGaMnO: the lattice parameter almost linearly decreases from 1.5 K to and then monotonically increases up to 873 K (almost linearly from 300 K); the parameter monotonically increases from 1.5 to 300 K and then decreases up to 600 K.

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Source
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9472281PMC
http://dx.doi.org/10.1021/acs.inorgchem.2c02343DOI Listing

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