Abstract
The magnetic structure of and multiferroics has been studied by high-pressure neutron diffraction in a large pressure range up to 6.6 GPa. In both cases, we observe a pressure-induced commensurate magnetic phase with propagation vector , growing with pressure at the expense of the ambient pressure phases. Being previously observed in and , this phase is most likely a generic feature of the multiferroic family. A simple model is proposed to explain qualitatively the emergence of this pressure-induced phase. Differences between and behaviors at ambient and low pressures provide clues on the interaction scheme.
5 More- Received 20 April 2018
DOI:https://doi.org/10.1103/PhysRevB.98.024408
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