FeCr2S4 in magnetic fields: Possible evidence for a multiferroic ground state
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BERTINSHAW, Joel, ULRICH, Clemens, GUNTHER, A., SCHRETTLE, Florian, WOHLAUER, M., KROHNS, Stephan, REEHUIS, Manfred, STUDER, Andrew J., AVDEEV, M. Yu., QUACH, Dat V., GROZA, Joanna R., TSURKAN, Vladimir, LOIDL, Alois. FeCr2S4 in magnetic fields: Possible evidence for a multiferroic ground state. In: Scientific Reports, 2014, vol. 4, pp. 1-8. ISSN 2045-2322. DOI: https://doi.org/10.1038/srep06079
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Scientific Reports
Volumul 4 / 2014 / ISSN 2045-2322

FeCr2S4 in magnetic fields: Possible evidence for a multiferroic ground state

DOI:https://doi.org/10.1038/srep06079

Pag. 1-8

Bertinshaw Joel12, Ulrich Clemens12, Gunther A.3, Schrettle Florian3, Wohlauer M.3, Krohns Stephan3, Reehuis Manfred4, Studer Andrew J.2, Avdeev M. Yu.2, Quach Dat V.5, Groza Joanna R.5, Tsurkan Vladimir36, Loidl Alois3
 
1 University of New South Wales,
2 Australian Nuclear Science and Technology Organisation, Lucas Heights,
3 Center for Electronic Correlations and Magnetism, University of Augsburg,
4 Helmholtz-Zentrum Berlin für Materialien und Energie,
5 University of California at Davis,
6 Institute of Applied Physics, Academy of Sciences of Moldova
 
 
Disponibil în IBN: 26 septembrie 2023


Rezumat

We report on neutron diffraction, thermal expansion, magnetostriction, dielectric, and specific heat measurements on polycrystalline FeCr 2S4 in external magnetic fields. The ferrimagnetic ordering temperatures TC ≈ 170K and the transition at T OO ≈ 10K, which has been associated with orbital ordering, are only weakly shifted in magnetic fields up to 9T. The cubic lattice parameter is found to decrease when entering the state below TOO. The magnetic moments of the Cr- and Fe-ions are reduced from the spin-only values throughout the magnetically ordered regime, but approach the spin-only values for fields >5.5T. Thermal expansion in magnetic fields and magnetostriction experiments indicate a contraction of the sample below about 60K. Below TOO this contraction is followed by a moderate expansion of the sample for fields larger than ∼4.5T. The transition at TOO is accompanied by an anomaly in the dielectric constant. The dielectric constant depends on both the strength and orientation of the external magnetic field with respect to the applied electric field for T < TOO. A linear correlation of the magnetic-field-induced change of the dielectric constant and the magnetic-field dependent magnetization is observed. This behaviour is consistent with the existence of a ferroelectric polarization and a multiferroic ground state below 10K.

Cuvinte-cheie
magnetism, Curie Temperature, Antiferromagnet