Abstract
Inelastic neutron scattering measurements of the magnetic excitations in indicate that the spin wave velocity in the Fe layers is exceptionally large and similar in magnitude to the cuprates. However, the spin wave velocity perpendicular to the layers is at least half as large that in the layer, so that the magnetism is more appropriately categorized as anisotropic three-dimensional, in contrast to the two-dimensional cuprates. Exchange constants derived from band structure calculations predict spin wave velocities that are consistent with the experimental data.
- Received 10 September 2008
DOI:https://doi.org/10.1103/PhysRevLett.101.227205
©2008 American Physical Society