Pressure-induced charge orders and their postulated coupling to magnetism in hexagonal multiferroic LuFe2O4

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作者
Fengliang Liu
Yiqing Hao
Jinyang Ni
Yongsheng Zhao
Dongzhou Zhang
Gilberto Fabbris
Daniel Haskel
Shaobo Cheng
Xiaoshan Xu
Lifeng Yin
Hongjun Xiang
Jun Zhao
Xujie Lü
Wenbin Wang
Jian Shen
Wenge Yang
机构
[1] Fudan University,State Key Laboratory of Surface Physics and Department of Physics
[2] Center for High Pressure Science and Technology Advanced Research (HPSTAR),Department of Physics
[3] Nanchang University,Hawaii Institute of Geophysics & Planetology
[4] University of Hawaii Manoa,Advanced Photon Source
[5] Argonne National Laboratory,Department of Condensed Matter Physics and Materials Science
[6] Brookhaven National Laboratory,Department of Physics and Astronomy
[7] University of Nebraska,Institute for Nanoelectronic Devices and Quantum Computing
[8] Fudan University,undefined
[9] Collaborative Innovation Center of Advanced Microstructures,undefined
[10] Shanghai Qi Zhi Institute,undefined
[11] Shanghai Research Center for Quantum Sciences,undefined
来源
npj Quantum Materials | / 8卷
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摘要
Hexagonal LuFe2O4 is a promising charge order (CO) driven multiferroic material with high charge and spin-ordering temperatures. The coexisting charge and spin orders on Fe3+/Fe2+ sites result in magnetoelectric behaviors, but the coupling mechanism between the charge and spin orders remains elusive. Here, by tuning external pressure, we reveal three charge-ordered phases with suggested correlation to magnetic orders in LuFe2O4: (i) a centrosymmetric incommensurate three-dimensional CO with ferrimagnetism, (ii) a non-centrosymmetric incommensurate quasi-two-dimensional CO with ferrimagnetism, and (iii) a centrosymmetric commensurate CO with antiferromagnetism. Experimental in situ single-crystal X-ray diffraction and X-ray magnetic circular dichroism measurements combined with density functional theory calculations suggest that the charge density redistribution caused by pressure-induced compression in the frustrated double-layer [Fe2O4] cluster is responsible for the correlated spin-charge phase transitions. The pressure-enhanced effective Coulomb interactions among Fe-Fe bonds drive the frustrated (1/3, 1/3) CO to a less frustrated (1/4, 1/4) CO, which induces the ferrimagnetic to antiferromagnetic transition. Our results not only elucidate the coupling mechanism among charge, spin, and lattice degrees of freedom in LuFe2O4, but also provide a new way to tune the spin-charge orders in a highly controlled manner.
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