Abstract
We present a systematic x-ray magnetic circular dichroism (XMCD) study performed at the rare-earth edges in Laves phase compounds. The progressive substitution of Al by Fe reveals the existence of a non-negligible contribution of Fe to the rare-earth XMCD spectra. This contribution has been isolated and shown to be similar to the dichroic spectrum recorded at the Fe edge. These results open the possibility of monitoring the Fe magnetism in lanthanides-iron intermetallic compounds by probing the rare-earth -edge x-ray absorption edges.
- Received 6 July 2005
DOI:https://doi.org/10.1103/PhysRevB.72.052412
©2005 American Physical Society