Valence delocalization and crystal structure of [Fe3O(pazo)(6)(py)(3)]center dot 3py: An example of the mixed valence delocalization between two ironatoms
M. Manago et al., Valence delocalization and crystal structure of [Fe3O(pazo)(6)(py)(3)]center dot 3py: An example of the mixed valence delocalization between two ironatoms, B CHEM S J, 72(10), 1999, pp. 2229-2234
The oxo-centered, trinuclear, mixed-valence complex [Fe3O(pazo)(6)(py)(3)].
3py, where pazo is 4-phenylazobenzoic acid, has been prepared, and the int
ramolecular electron transfer properties in the solid state have been studi
ed. There are two doublets in the area ratio of two (Fe3+) and one (Fe2+) a
t 78 K. Increasing the sample temperature above 120 K turns these to two do
ublets in the area ratio of two (Fe2.5+) and one (Fe3+); the average valenc
e state between an iron(II) and one of two irons(III) is observed. The comp
lex crystallizes in the C-centered monoclinic space group C2/c with 4 molec
ules in a unit cell which has dimensions: a = 15.856(4), b = 28.649(2), c =
25.739(2) Angstrom, V = 11317(3) Angstrom(3), beta = 104.54(1) at 150 K, a
nd a = 15.867(3), b = 28.555(3), c = 25.747(5) Angstrom, V = 11288(3) Angst
rom(3), beta = 104.60(2) at 85 K. The metal sites of the average valence st
ate and Fe3+ state are seen in its single-crystal X-ray structure at both t
emperatures. The X-ray structure work shows that the dimensions of the Fe3O
triangle become larger and the length of b-axis becomes longer with increa
sing of temperature. There is a C-2 axis in the molecule, Fe-B(3+) and a py
ridine coordinating to the Fe-B(3+) being located on the axis. The plane of
the pyridine is almost perpendicular to that of the Fe3O triangle and thos
e of other two pyridines coordinating to Fe2.5+ (Fe2+ + Fe-A(3+)) are paral
lel to that of the Fe3O triangle.