Large spin-driven dielectric response and magnetoelectric coupling in the buckled honeycomb Fe4 Nb2 O9

Lei Ding, Minseong Lee, Eun Sang Choi, Jing Zhang, Yan Wu, Ryan Sinclair, Bryan C. Chakoumakos, Yisheng Chai, Haidong Zhou, Huibo Cao

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11 Scopus citations

Abstract

We present the significant spin-driven dielectric anomaly (∼40% drop) and magnetoelectric coupling near the magnetic ordering temperature in single crystal Fe4Nb2O9. By combining neutron and x-ray single crystal diffraction techniques, we unambiguously determined its magnetic symmetry and studied the structural phase transition at TS = 70 K. The temperature-dependent static dielectric constant is strongly anisotropic, rendering two dielectric anomalies along the a axis in the hexagonal lattice with the first one coupled to the magnetic ordering around TN = 97 K and the second one accompanying with a first-order structural transition around TS = 70 K. Below TN, we found that the anomalous dielectric constant is practically proportional to the square of the magnetic moment from neutron diffraction data, indicating that the exchange striction is likely responsible for the strong spin-lattice coupling. Magnetic-field-induced magnetoelectric coupling was observed and is compatible with the determined magnetic structure that is characteristic of antiferromagnetically arranged ferromagnetic chains in the honeycomb plane. We propose that such magnetic symmetry should be immune to external magnetic fields to some extent favored by the freedom of rotation of moments in the honeycomb plane, laying out a promising system to control the magnetoelectric properties by magnetic fields.

Original languageEnglish
Article number084403
JournalPhysical Review Materials
Volume4
Issue number8
DOIs
StatePublished - Aug 2020

Funding

The research at Oak Ridge National Laboratory (ORNL) was supported by the U.S. Department of Energy (DOE), Office of Science, Office of Basic Energy Sciences, Early Career Research Program Award KC0402010, under Contract DE-AC05-00OR22725. This research used resources at the High Flux Isotope Reactor, a DOE Office of Science User Facility operated by ORNL. The work at the University of Tennessee was supported by DOE under award DE-SC-0020254. A portion of this work was performed at the National High Magnetic Field Laboratory, supported by the National Science Foundation Cooperative Agreement No. DMR-1644779 and the State of Florida. The work at Chongqing University was supported by the Fundamental Research Funds for the Central Universities (2020CDJQY-A056, 2018CDJDWL0011) and Projects of President Foundation of Chongqing University (2019CDXZWL002).

FundersFunder number
DOE Office of Science
Office of Basic Energy Sciences
State of Florida
National Science FoundationDMR-1644779
U.S. Department of Energy
Office of Science
Basic Energy SciencesDE-AC05-00OR22725, DE-SC-0020254, KC0402010
Oak Ridge National Laboratory
Chongqing University2019CDXZWL002
Fundamental Research Funds for the Central Universities2020CDJQY-A056, 2018CDJDWL0011

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