4.5 Article

Magnetic properties of multiferroic Pb5Fe3F19

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ELSEVIER
DOI: 10.1016/j.jmmm.2021.168540

Keywords

Pb5Fe3F19; Multiferroicity; Ferromagnetism; Ferroelectricity; Magnetoelectric coupling

Funding

  1. National Natural Science Foundation of China [51771053, 51971109]
  2. Natural Science Foundation of Jiangsu Province of China [BK20201285]
  3. National Key Research and Development Program of China [2016YFA0300803]
  4. Funda-mental Research Funds for the Central Universities [2242020k30039]
  5. open research fund of Key Laboratory of MEMS of Ministry of Education, Southeast University

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Fluoride ferroelectrics containing 3d transition metal ions show potential as single-phase multiferroics. The study successfully prepared pure phase Pb5Fe3F19 powders with confirmed ferroelectricity and magnetoelectric coupling. Two antiferromagnetic transitions were observed at different temperatures, along with the existence of weak ferromagnetism.
Fluoride ferroelectrics containing 3d transition metal ions are potential single-phase multiferroics. Pure phase Pb5Fe3F19 powders are prepared by the solid-state reaction, which is confirmed by the X-ray diffraction with isostructure to Pb5Cr3F19. X-ray photoelectron spectroscopy confirms that Fe ions are in the valence state of +3. Ferroelectricity is confirmed by the observation of amplitude and phase hysteresis loops by piezoresponse force microscopy at room temperature. Two anomalies are observed at T-N1 of 78 K and T-N2 of 21 K in the temperature dependent magnetization (M -T) curves, which is due to the onset of two antiferromagnetic transitions. The bifurcation between the zero-field cooled and field cooled M -T curves at temperatures below T-N1 of 78 K is attributed to competition of the complicated antiferromagnetic exchange coupling between the neighboring Fe3+ ions, leading to the magnetic relaxation. Small hysteresis with negligible coercivity can be observed in the field dependent magnetization curves below T-N1. The magnetization and coercivity are significantly enhanced with further decreasing temperature, indicating the weak ferromagnetism. The observed ferromagnetism might be due to the magnetoelectric coupling between the ferroelectric polarization and magnetization, leading to the spin canting of the antiferromagnetic coupling between neighboring Fe3+ ions. The magnetoelectric coupling is confirmed by the observation of magnetodielectric effect, which is due to the strong magnetic and structural coupling.

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