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Anisotropic Thermal Expansion and a Second-Order Charge Order Transition in the Ferrimagnetic Dy2CuZnMn4O12 Perovskite with Triple A-Site Cation Ordering.


ABSTRACT: Dy2CuZnMn4O12 perovskite, belonging to the A-site columnar-ordered quadruple perovskite family with the general composition of A2A'A″B4O12, was prepared by a high-pressure, high-temperature method at 6 GPa and 1500 K. Its crystal structure was studied by synchrotron powder X-ray diffraction between 100 and 800 K. The ideal cation distribution (without antisite disorder) was found to be realized within the sensitivity of the synchrotron X-ray diffraction method. Between 100 and 400 K, it crystallizes in space group Pmmn (no. 59) and has layered charge ordering of Mn3+ and Mn4+ at the B sites. Above 425 K, it crystallizes in space group P42/nmc (no. 137) with one crystallographic B site and an average Mn3.5+ oxidation state. The charge ordering transition (at TCO = 425 K) appears to be of the second order as no anomalies were found on differential scanning calorimetry curves and temperature dependence of the unit cell volume, and the orthorhombic a and b lattice parameters merge gradually. The compound demonstrates anisotropic thermal expansion with the c lattice parameter decreasing with increasing temperature above 280 K. A ferrimagnetic transition occurs at TC = 116 K with an additional, gradual rise of magnetic susceptibilities below 45 K, probably due to increases of the ordered moments of the Dy sublattices.

SUBMITTER: Belik AA 

PROVIDER: S-EPMC10910486 | biostudies-literature | 2023 Dec

REPOSITORIES: biostudies-literature

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Anisotropic Thermal Expansion and a Second-Order Charge Order Transition in the Ferrimagnetic Dy<sub>2</sub>CuZnMn<sub>4</sub>O<sub>12</sub> Perovskite with Triple A-Site Cation Ordering.

Belik Alexei A AA  

Inorganic chemistry 20231127 49


Dy<sub>2</sub>CuZnMn<sub>4</sub>O<sub>12</sub> perovskite, belonging to the A-site columnar-ordered quadruple perovskite family with the general composition of A<sub>2</sub>A'A″B<sub>4</sub>O<sub>12</sub>, was prepared by a high-pressure, high-temperature method at 6 GPa and 1500 K. Its crystal structure was studied by synchrotron powder X-ray diffraction between 100 and 800 K. The ideal cation distribution (without antisite disorder) was found to be realized within the sensitivity of the synchr  ...[more]

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