Abstract
Crystallographic and morphologic features of quadruple and double superstructures in with were investigated by x-ray powder diffraction and transmission electron microscopy. The presence of a quadruple superstructure accompanied by antiferroic ionic displacements was found near the morphotropic phase boundary between the phase () and the Pnma phase (). The quadruple superlattice phase coexists with a ferroelectric phase at . These superstructures were found to originate from the freezing of multiple phonon modes related to transverse wave ionic displacements. These findings provide further insight towards understanding the complexity of rare-earth-doped .
- Received 3 March 2019
- Revised 14 June 2019
DOI:https://doi.org/10.1103/PhysRevB.100.024105
©2019 American Physical Society