Abstract / Description of output
Long range ordering of two transition metal charge (oxidation) states occurs in many oxides. Direct structural evidence from powder neutron diffraction studies on several half-doped manganites (Pr0.5Ca0.5MnO3, TbBaMn2O6, YBaMn2O6) and magnetite (Fe3O4) is reviewed. Charge ordering is accompanied by subtle distortions to low (monoclinic or triclinic) symmetry in all cases. The half-doped manganites reveal polymorphism of both charge and Mn3+ orbital ordered arrangements. The degree of charge separation estimated by bond valence sums for these and other oxides is only 20-80% of the ideal difference. The origin of this effect is not clear from present data. (c) 2006 Elsevier SAS. All rights reserved.
Original language | English |
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Pages (from-to) | 861-867 |
Number of pages | 7 |
Journal | Solid state sciences |
Volume | 8 |
Issue number | 8 |
DOIs | |
Publication status | Published - Aug 2006 |
Keywords / Materials (for Non-textual outputs)
- LOW-TEMPERATURE STRUCTURE
- VERWEY TRANSITION
- ROOM-TEMPERATURE
- MAGNETITE FE3O4
- PHASE
- DISPROPORTIONATION
- DIFFRACTION
- MANGANITES
- SCATTERING
- VALENCE