Direct observation of t2g orbital ordering in magnetite
arXiv:cond-mat/0605096 · doi:10.1103/PhysRevLett.100.026406
Abstract
Using soft-x-ray diffraction at the site-specific resonances in the Fe L23 edge, we find clear evidence for orbital and charge ordering in magnetite below the Verwey transition. The spectra show directly that the (001/2) diffraction peak (in cubic notation) is caused by t2g orbital ordering at octahedral Fe2+ sites and the (001) by a spatial modulation of the t2g occupation.
to appear in Phys. Rev. Lett