Abstract
By comprehensive neutron diffraction measurements we have studied the magnetic structure of aegirine in and above its multiferroic phase. Natural aegirine exhibits two magnetic transitions into incommensurate magnetic order with a propagation vector of . Between 9 and 6 K, we find a transverse spin-density wave with moments pointing near the direction. Below 6 K, magnetic order becomes helical and spins rotate in the plane. The same irreducible representation is involved in the two successive transitions. In addition, the ferroelectric polarization appearing along the direction cannot be described by the most common multiferroic mechanism but follows . Synthetic does not exhibit the pure incommensurate helical order but shows coexistence of this order with a commensurate magnetic structure. By applying moderate pressure to natural aegirine, we find that the incommensurate magnetic ordering partially transforms to the commensurate one, underlining the nearly degenerate character of the two types of order in .
4 More- Received 26 March 2015
- Revised 12 May 2015
DOI:https://doi.org/10.1103/PhysRevB.91.214415
©2015 American Physical Society