Hyperfine Interact DOI 10.1007/s10751-013-0973-8 Iron orbital occupancies upon valence mixing of charge-ordered GdBaFe II Fe III O 5 J. Lind´ en · F. Lindroos · P. Karen © Springer Science+Business Media Dordrecht 2013 Abstract ossbauer spectra of charge-ordered/valence-mixed GdBaFe 2 O 5 have been ana- lyzed in order to determine the orbital occupancies of the minority-spin d electron as a function of temperature. In the charge-ordered state below the Verwey temperature T V , it occupies the Fe 2+ d xz orbital, which is ordered. Above T V , the electron partially occurs also at the trivalent iron and spreads over two additional orbitals, d x 2 y 2 and d z 2 . In the valence-mixing state (above T p ) also orbital d yz participates. The study illustrates how the M¨ ossbauer electric-field gradient, center shift and internal field jointly reflect the distribution of the minority-spin electron culprit behind the Verwey transition. Keywords 57 Fe M¨ ossbauer spectroscopy · Charge ordering · Valence mixing · Mixed valence · Double perovskites 1 Introduction The antiferromagnetic A-site ordered perovskite RBaFe 2 O 5 (R is a rare-earth element) contains Fe 2+ and Fe 3+ that order at low temperatures and mix at high temperatures [1]. The valence mixing proceeds in two steps [2], where the first one, at the lower transi- tion temperature T V , has all features of the Verwey transition [3] in magnetite. Above the second transition temperature T p , iron is in a single valence state Fe 2.5+ . At low tem- peratures, a long-range order of alternating chains of di- and trivalent iron coordinations along b (Fig. 1) is observed by neutron- [2] and synchrotron X-ray powder diffraction [4]. Proceedings of the 32nd International Conference on the Applications of the M ¨ ossbauer Effect (ICAME 2013) held in Opatija, Croatia, 1–6 September 2013 J. Lind´ en () · F. Lindroos Physics Department, ˚ Abo Akademi University, 20500 Turku, Finland e-mail: jlinden@abo.fi P. Karen Department of Chemistry, University of Oslo, 0315 Oslo, Norway