Abstract
The indirect coupling between Ni-O-Ni chains of the phase nickelates rare earth) results in a range of interesting magnetic behavior. In this work Mössbauer spectroscopy data for K) are interpreted in terms of a constant electric-field gradient tensor and a temperature-dependent magnetic hyperfine field with a saturation value of T. The sensitivity of the spectra to the projection of the hyperfine field enables a magnetic feature at K to be identified with magnetic reorientation from the a to the b axis. These results assist with the characterization of the crystal-field interaction for the Tm site in isostructural (the first such characterization for this particular structural series).
- Received 10 August 1999
DOI:https://doi.org/10.1103/PhysRevB.61.6220
©2000 American Physical Society