Abstract
Based on the detailed Mn -edge x-ray resonant scattering results, we report a new complexity in the magnetic order of multiferroic orthomangnites, which has been considered as the simple -type cycloid order inducing ferroelectricity. The Dzyaloshinskii-Moriya interaction involved in the orthorhombic distortion brings on -type canting from the type, and the ordering type becomes the off-phase synchronized cycloid in or the tilted antiphase cycloid in . The -type canting is responsible for the magnetic field-driven multiferroicity to weak ferromagnetism transition.
- Received 12 August 2010
DOI:https://doi.org/10.1103/PhysRevLett.106.047203
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