Abstract
Transmission-electron microscopy has shown that the strongly piezoelectric material separates into two phases at low temperatures. The majority phase is the monoclinic phase previously found by x-ray diffraction. The minority phase, with a nanoscale coherence length, is a slightly distorted variant of the first resulting from the antiphase rotation of the oxygen octahedra about [111]. This work clears up a recent controversy about the origin of superlattice peaks in these materials, and supports recent theoretical results predicting the coexistence of ferroelectric and rotational instabilities.
- Received 24 April 2002
DOI:https://doi.org/10.1103/PhysRevB.66.060103
©2002 American Physical Society