1802
N. Masuhara et al. / Polyhedron 24 (2005) 1798–1802
compared to ferrocene (2.4 mm sꢁ1) is explained by the
interaction of the e2g d orbitals with the ring orbitals [8].
Although the X-ray crystal structural analyses showed
that the two iron sites are slightly different in the dinuclear
o- and m-terphenyl complexes, the slight difference in the
site does not appear in the Mo¨ssbauer spectra. And the
difference between the mononuclear and the dinuclear
complexes does not significantly appear in the 57Fe Mo¨ss-
bauer spectra. Close inspection, however, reveals that o-
terphenyl complexes show slightly larger QS value.
(fax: +44 1223 336033; e-mail: deposit@ccdc.cam.ac.uk
data associated with this article can be found, in the
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Appendix A. Supplementary data
Crystallographic data for the structural analysis have
been deposited at the Cambridge Crystallographic Data
Centre, CCDC 249481–249485. Copies of this informa-
tion may be obtained free of charge from the Director,
CCDC, 12 Union Road, Cambridge CB2 1EZ, UK