Abstract
We study the effect of hydrostatic pressure on the electrical transport, magnetic, and structural properties of MnBi2Te4 by measuring its resistivity, Hall effect, and x-ray diffraction under pressures up to 12.8 GPa supplemented by the first-principles calculations. At ambient pressure, MnBi2Te4 shows a metallic conducting behavior with a cusplike anomaly at around TN≈24K, where it undergoes a long-range antiferromagnetic (AF) transition. With increasing pressure, TN determined from the resistivity anomaly first increases slightly with a maximum at around 2 GPa and then decreases until vanishing completely at about 7 GPa. Intriguingly, its resistivity is enhanced gradually by pressure and even evolves from metallic to semimetal or semiconductinglike behavior as TN is suppressed. However, the density of the n-type charge carrier that remains dominant under pressure increases with pressure. In addition, the interlayer AF coupling seems to be strengthened under compression, since the critical field Hc1 for the spin-flop transition to the canted AF state is found to increase with pressure. No structural transition was evidenced up to 12.8 GPa, but some lattice softening was observed at about 2 GPa, signaling the occurrence of an electronic transition or crossover from a localized to itinerant state. We have rationalized these experimental findings by considering the pressure-induced enhancement of antiferromagnetic/ferromagnetic competition and partial delocalization of Mn-3d electrons, which not only destroys long-range AF order but also promotes charge-carrier localization through enhanced spin fluctuations and/or the formation of a hybridization gap at high pressure.
Original language | English |
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Article number | 094201 |
Journal | Physical Review Materials |
Volume | 3 |
Issue number | 9 |
DOIs | |
State | Published - Sep 3 2019 |
Bibliographical note
Publisher Copyright:© 2019 American Physical Society.
Funding
This work is supported by the National Key R&D Program of China (Grants No. 2018YFA0305700 and No. 2018YFA0305800), the National Natural Science Foundation of China (Grants No. 11574377, No. 11888101, No. 11834016, and No. 11874400), the Strategic Priority Research Program and Key Research Program of Frontier Sciences of the Chinese Academy of Sciences (Grants No. XDB25000000 and No. QYZDB-SSW-SLH013), as well as the CAS Interdisciplinary Innovation Team. J.Q.Y. and D.S.P. are supported by the U.S. Department of Energy, Office of Science, Basic Energy Sciences, Materials Sciences and Engineering Division. J.S.Z. is supported by the National Science Foundation through Grant No. DMR-1729588. This work is supported by the National Key R&D Program of China (Grants No. 2018YFA0305700 and No. 2018YFA0305800), the National Natural Science Foundation of China (Grants No. 11574377, No. 11888101, No. 11834016, and No. 11874400), the Strategic Priority Research Program and Key Research Program of Frontier Sciences of the Chinese Academy of Sciences (Grants No. XDB25000000 and No. QYZDB-SSW-SLH013), as well as the CAS Interdisciplinary Innovation Team. J.Q.Y. and D.S.P. are supported by the U.S. Department of Energy, Office of Science, Basic Energy Sciences, Materials Sciences and Engineering Division. J.S.Z. is supported by the National Science Foundation through Grant No. DMR-1729588.
Funders | Funder number |
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National Key R&D Program of China | |
National Science Foundation | DMR-1729588 |
U.S. Department of Energy | |
Directorate for Mathematical and Physical Sciences | 1729588 |
Office of Science | |
Basic Energy Sciences | |
Division of Materials Sciences and Engineering | |
National Natural Science Foundation of China | 11888101, 11874400, 11574377, 11834016 |
Chinese Academy of Sciences | XDB25000000 |
National Key Research and Development Program of China | 2018YFA0305800, 2018YFA0305700 |