Abstract
The ferroelectromagnet consists of weakly coupled triangular layers of spins. Below muon-spin relaxation data show two oscillatory relaxing signals due to magnetic order, with no purely relaxing signals resolvable (which would require different coexisting spin distributions). The transition temperature increases with applied hydrostatic pressure, even though the ordered moment decreases. These results suggest that pressure increases both the exchange coupling between the layers and the frustration within the layers.
- Received 17 October 2006
DOI:https://doi.org/10.1103/PhysRevLett.98.197203
©2007 American Physical Society