Abstract
Multiferroic orthorhombic exhibits large ferroelectric polarization induced by an -type magnetic order. Recently, the -type magnetic phase in was proposed to feature magnetic moments tilted away from the collinear ordering. We employed neutron diffraction to determine the symmetry of the magnetic order in . We observed that below K, the spins order into an incommensurate amplitude-modulated phase that obeys the Pbnm crystal symmetry and is paraelectric. The incommensurate phase locks into a commensurate phase at K described by a fully antiferromagnetic and noncollinear -type order. This noncollinear -type ordering breaks the spatial inversion symmetry and induces a spontaneous polarization at . At K, an appreciably large electric polarization was observed similar to that of other orthorhombic manganites featuring -type magnetic order. We also present a Pbnm symmetry-allowed Dzyaloshinskii-Moriya interaction that explains the noncollinear -type order in the commensurate phase. These results are in qualitative agreement with the type of distortions from collinear -type antiferromagnetic order found using Monte Carlo simulation for rare-earth manganites [M. Mochizuki et al., Phys. Rev. B 84, 144409 (2011)].
2 More- Received 20 September 2016
DOI:https://doi.org/10.1103/PhysRevB.95.104412
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