High-Pressure Synthesis and Ferrimagnetic Ordering of the B-Site-Ordered Cubic 
Perovskite Pb2FeOsO6

Zhao, Qing; Liu, Min; Dai, Jianhong; Yin, Yunyu; Zhou, Long; Yang, Junye; Hu, Zhiwei; Agrestini, Stefano; Chen, Kai; Pellegrin, Eric; Valvidares, Manuel; Nataf, Lucie; Baudelet, Francois; Tjeng, L. H.; Yang, Yi-feng; Jin, Changqing; Long, Youwen

doi:10.1021/acs.inorgchem.6b01649

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High-Pressure Synthesis and Ferrimagnetic Ordering of the B-Site-Ordered Cubic Perovskite Pb₂FeOsO₆

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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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Agrestini, Stefano
Stefano Agrestini, Physics of Correlated Matter, Max Planck Institute for Chemical Physics of Solids, Max Planck Society;

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

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Citation

Zhao, Q., Liu, M., Dai, J., Yin, Y., Zhou, L., Yang, J., et al. (2016). High-Pressure Synthesis and Ferrimagnetic Ordering of the B-Site-Ordered Cubic Perovskite Pb₂FeOsO₆. Inorganic Chemistry, 55(19), 9816-9821. doi:10.1021/acs.inorgchem.6b01649.

Cite as: https://hdl.handle.net/11858/00-001M-0000-002B-B9F0-9

Abstract

Pb2FeOsO6 was prepared for the first time by using high-pressure and high-temperature synthesis techniques. This compound crystallizes into a B-site-ordered double-perovskite structure with cubic symmetry Fm (3) over barm, where the Fe and Os atoms are orderly distributed with a rock-salt-type manner. Structure refinement shows an Fe-Os antisite occupancy of about 16.6%. Structural analysis and X-ray absorption spectroscopy both demonstrate the charge combination to be Pb2Fe3+Os5+O6. A long-range ferrimagnetic transition is found to occur at about 280 K due to antiferromagnetic interactions between the adjacent Fe3+ and Os5+ spins with a straight (180 degrees) Fe-O-Os bond angle, as confirmed by X-ray magnetic circular-dichroism measurements. First-principles theoretical calculations reveal the semiconducting behavior as well as the Fe3+(up arrow)Os5+(down arrow,) antiferromagnetic coupling originating from the superexchange interactions between the half-filled 3d orbitals of Fe and t(2g) orbitals of Os.