Resonant x-ray scattering was used to investigate electronic fluctuations o
f the octahedral iron atoms in magnetite. We measured the (002) and (006) "
forbidden" x-ray diffraction reflections permitted by the anisotropy of the
iron anomalous scattering factor. The energy and azimuthal angle dependenc
ies of these reflections, and the polarization analysis, an shown and discu
ssed. The results clearly show p and d iron empty states ordering in magnet
ite at room temperature. Moreover, the octahedral iron atoms an electronica
lly equivalent in a time scale lower than 10(-16) sec. Therefore, magnetite
should be considered as an itinerant magnet and not as a fluctuating mixed
valence material.