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High-Pressure Synthesis of a B-site Co2+/Mn4+Disordered Quadruple Perovskite LaMn3Co2Mn2O12

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Tjeng,  Liu-Hao
Liu Hao Tjeng, Physics of Correlated Matter, Max Planck Institute for Chemical Physics of Solids, Max Planck Society;

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Hu,  Zhiwei
Zhiwei Hu, Physics of Correlated Matter, Max Planck Institute for Chemical Physics of Solids, Max Planck Society;

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Citation

Guo, J., Shen, X., Liu, Z., Qin, S., Wang, W., Ye, X., et al. (2020). High-Pressure Synthesis of a B-site Co2+/Mn4+Disordered Quadruple Perovskite LaMn3Co2Mn2O12. Inorganic Chemistry, 59, 12445-12452. doi:10.1021/acs.inorgchem.0c01548.


Cite as: http://hdl.handle.net/21.11116/0000-0007-0E40-2
Abstract
A new oxide, LaMn3Co2Mn2O12, was synthesized under high-pressure (7 GPa) and high-temperature (1423 K) conditions. The compound crystallizes in an AA′3B4O12-type quadruple perovskite structure with space group Im3¯. The Rietveld structural analysis combined with soft X-ray absorption spectroscopy reveals the charge combination to be LaMn3+3Co2+2Mn4+2O12, where the La3+ and Mn3+ are 1:3 ordered respectively at the A and A′ sites, whereas the Co2+ and Mn4+ are disorderly distributed at the B site. This is in sharp contrast to R2Co2+Mn4+O6 (R = La and rare earth) double perovskites, in which the Co2+ and Mn4+ charge states are always orderly distributed with a rocksalt-type fashion, giving rise to a long-range magnetic ordering. As a result, LaMn3Co2Mn2O12 displays spin glassy magnetic properties due to the random Co2+ and Mn4+ distribution, as demonstrated by dc and ac magnetic susceptibility as well as specific heat measurements. Possible factors that affect the B-site degree of order in perovskite structures are discussed. © 2020 American Chemical Society.