biostudies-literatureUnknown62(49)Belik AADy₂CuZnMn₄O₁₂ 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 <i>Pmmn</i> (no. 59) and has layered charge ordering of Mn³⁺ and Mn⁴⁺ at the B sites. Above 425 K, it crystallizes in space group <i>P</i>4₂/<i>nmc</i> (no. 137) with one crystallographic B site and an average Mn^3.5+ oxidation state. The charge ordering transition (at <i>T</i>_CO = 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 <i>a</i> and <i>b</i> lattice parameters merge gradually. The compound demonstrates anisotropic thermal expansion with the <i>c</i> lattice parameter decreasing with increasing temperature above 280 K. A ferrimagnetic transition occurs at <i>T</i>_C = 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.Inorganic chemistry20042-20049https://www.ebi.ac.uk/biostudies/studies/S-EPMC10910486biostudies-literatureAnisotropic Thermal Expansion and a Second-Order Charge Order Transition in the Ferrimagnetic Dy₂CuZnMn₄O₁₂ Perovskite with Triple A-Site Cation Ordering.PMC10910486Belik AAfalseAnisotropic Thermal Expansion and a Second-Order Charge Order Transition in the Ferrimagnetic Dy₂CuZnMn₄O₁₂ Perovskite with Triple A-Site Cation Ordering.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 <i>Pmmn</i> (no. 59) and has layered charge ordering of Mn³⁺ and Mn⁴⁺ at the B sites. Above 425 K, it crystallizes in space group <i>P</i>4₂/<i>nmc</i> (no. 137) with one crystallographic B site and an average Mn^3.5+ oxidation state. The charge ordering transition (at <i>T</i>_CO = 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 <i>a</i> and <i>b</i> lattice parameters merge gradually. The compound demonstrates anisotropic thermal expansion with the <i>c</i> lattice parameter decreasing with increasing temperature above 280 K. A ferrimagnetic transition occurs at <i>T</i>_C = 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.2023-01-01T00:00:00Z2023 Dec2025-04-05T11:38:55.226Z2025-04-05T11:38:55.226ZS-EPMC109104863801286010.1021/acs.inorgchem.3c02835