Direct observation of t 2g orbital ordering in magnetite
Using soft-x-ray diffraction at the site-specific resonances in the Fe L2,3 edge, we find clear evidence for orbital and charge ordering in magnetite below the Verwey transition. The spectra show directly that the (0012) diffraction peak (in cubic notation) is caused by t2g orbital ordering at octah...
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| Hauptverfasser: | , |
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| Dokumenttyp: | Article (Journal) |
| Sprache: | Englisch |
| Veröffentlicht: |
17 January 2008
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| In: |
Physical review letters
Year: 2008, Jahrgang: 100, Heft: 2 |
| ISSN: | 1079-7114 |
| DOI: | 10.1103/PhysRevLett.100.026406 |
| Online-Zugang: | Verlag, Volltext: http://dx.doi.org/10.1103/PhysRevLett.100.026406 Verlag, Volltext: https://link.aps.org/doi/10.1103/PhysRevLett.100.026406 
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| Verfasserangaben: | J. Schlappa, C. Schüßler-Langeheine, C.F. Chang, H. Ott, A. Tanaka, Z. Hu, M.W. Haverkort, E. Schierle, E. Weschke, G. Kaindl, and L.H. Tjeng |
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Direct observation of t2g orbital ordering in magnetite
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