A qualitative molecular orbital (MO) model for a dinuclear Fe(II)-Fe(III) c
omplex 2, which can be considered as two edge-sharing octahedra, is evaluat
ed on the basis of Extended-Huckel (EH) calculations. The MO picture derive
d is compared to the MO scheme suggested for a valence-delocalized Fe(II)-F
e(III) complex 1 studied recently, which represents two face-sharing octahe
dra. This comparison indicates that the iron-iron interaction plays an impo
rtant role in 1 while this interaction is weaker in 2. In both molecules va
lence delocalization is provided by an in-phase combination of iron-d-orbit
als of a-type with non-negligible ligand admixtures. The stronger intermeta
l coupling in 1 is mainly caused by the shorter iron-iron distance. (C) 199
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