Abstract
We have observed a weak anisotropic x-ray magnetic linear dichroism (AXMLD) at the Eu edges of ferromagnetic EuO(001), which indicates that the states are not rotationally invariant. A quantitative agreement of the AXMLD is obtained with multiplet calculations where the state is split by an effective cubic crystalline electrostatic field. The results indicate that the standard model of rare earths, where electrons are treated as core states, is not correct and that the orbitals contribute weakly to the magnetic anisotropy.
- Received 31 July 2007
- Corrected 15 February 2008
DOI:https://doi.org/10.1103/PhysRevLett.100.067403
©2008 American Physical Society
Corrections
15 February 2008