Abstract
(BMO), ferromagnetic (FM) below , was believed to also be ferroelectric (FE) due to a noncentrosymmetric structure, until diffraction data indicated that its space group is the centrosymmetric . Here we present infrared phonon spectra of BMO, taken on a mosaic of single crystals, which are consistent with at any , as well as room-temperature Raman data which strongly support this conclusion. We also find that the infrared intensity of several phonons increases steadily for , causing the relative permittivity of BMO to vary from 18.5 at 300 K to 45 at 10 K. At variance with FE materials of the displacive type, no appreciable softening has been found in the infrared phonons. Both their frequencies and intensities, moreover, appear insensitive to the FM transition at .
- Received 3 June 2015
- Revised 20 July 2015
DOI:https://doi.org/10.1103/PhysRevB.92.054306
©2015 American Physical Society