Abstract
We have successfully determined the hitherto unknown sign of the Stevens crystal-field parameter of the tetragonal heavy-fermion compound using vector -dependent nonresonant inelastic x-ray scattering experiments at the cerium edge. The observed difference between the two different directions, and , is due to the anisotropy of the crystal-field ground state in the (001) plane and is observable only because of the utilization of higher than dipole transitions possible in nonresonant inelastic x-ray scattering. This approach allows us to go beyond the specific limitations of dc magnetic susceptibility, inelastic neutron scattering, and soft x-ray spectroscopy, and provides us with a reliable information about the orbital state of the electrons relevant for the quantitative modeling of the quasiparticles and their interactions in heavy-fermion systems.
- Received 3 May 2012
DOI:https://doi.org/10.1103/PhysRevLett.109.046401
© 2012 American Physical Society