Abstract
57Fe Mössbauer spectroscopy was used to study the double perovskite GdBaFe2O5+w, which exhibits mixing of the integer valence states of iron. The valence mixing/separation process Fe2+ + Fe3+ ↔ 2Fe2.5+ was investigated as a function of temperature. For nearly stoichiometric compositions of w ≈ 0, a two-step Verwey-type transition is registered that separates Fe2.5+ into intermediate valence- and spin states Fe2.5-ε and Fe2.5+ε and then into the integer valences Fe2+ and Fe3+. Both steps are accompanied by a decrease in electrical conductivity, altogether by two orders of magnitude. Seebeck measurements identify holes as dominating charge carriers, with activation energy for hopping of ~0.10 eV in the valence-mixed state. It is inferred that the mixing electrons are not simply delocalized over the lattice, but rather form bridges connecting pairs of adjacent Fe atoms along the c axis.
| Original language | English |
|---|---|
| Pages (from-to) | 321-325 |
| Number of pages | 5 |
| Journal | Hyperfine Interactions |
| Volume | 156 |
| DOIs | |
| Publication status | Published - Dec 2004 |
| MoE publication type | A1 Journal article-refereed |
Keywords
- Fe Mössbauer spectroscopy
- Charge ordering
- Double perovskite
- Valence mixing
- Verwey-type transition