Abstract
We performed temperature dependent x-ray linear dichroism (XLD) experiments on an iron pnictide system, with , 0.05, 0.08, and 0.10 to experimentally verify the existence of orbital ordering (OO). Substantial XLD was observed in polarization dependent x-ray absorption spectra of Fe edges. By exploiting the difference in the temperature dependent behaviors, OO, and structure contributions to XLD could be clearly separated. The observed OO signal indicates different occupation numbers for and orbitals and supports the existence of ferro-OO. The results are also consistent with the theoretical prediction. Moreover, we find substantial OO signal well above the structural and magnetic transition temperatures, which suggests the existence of strong OO fluctuations up to high temperatures.
- Received 6 August 2013
- Corrected 18 December 2013
DOI:https://doi.org/10.1103/PhysRevLett.111.217001
© 2013 American Physical Society
Corrections
18 December 2013