AN X-RAY DETERMINATION OF THE ELECTRON-DISTRIBUTION IN CRYSTALS OF HEXAPYRIDINE-N-OXIDE COBALT(II) PERCHLORATE AND THE ELECTRONIC-STRUCTUREOF THE CO2+ ION
Js. Wood, AN X-RAY DETERMINATION OF THE ELECTRON-DISTRIBUTION IN CRYSTALS OF HEXAPYRIDINE-N-OXIDE COBALT(II) PERCHLORATE AND THE ELECTRONIC-STRUCTUREOF THE CO2+ ION, Inorganica Chimica Acta, 229(1-2), 1995, pp. 407-415
The valence electron density distribution in hexapyridine-N-oxide coba
lt(II) perchlorate, Co(C5H5NO)(6)(ClO4)(2), has been investigated expe
rimentally using high resolution single crystal X-ray diffraction data
collected at 78(1) K with Mo K alpha radiation, together with the res
ults from the already reported neutron structure determination. The cr
ystal data at 78 K are a=12.317(1) and c=18.826(1) Angstrom; space gro
up R (3) over bar, Z=3. Deformation electronic density maps have been
calculated from the X-ray data, using parameters from the refinement o
f the high order data, sin theta/lambda > 0.75 Angstrom(-1), the param
eters obtained from the refinement of the neutron data and from struct
ure factors obtained from a multipole deformation refinement. Conventi
onal spherical atom refinement on 4030 reflections (F-o greater than o
r equal to 3 sigma F-o) gives R=0.037 and R(w)=0.038, while the multip
ole refinement on 3627 reflections gives R=0.028 and R(w)=0.024. A pro
nounced aspherical electron distribution has been found for the cobalt
atom in the deformation maps which is consistent with a significant t
rigonal distortion of the distribution expected for an octahedral liga
nd field, viz. t(2g)(5.0) and e(g)(2.0). The populations obtained from
the multipole refinement confirm this and give apparent orbital occup
ancies of 3.7(1), 1.2(1) and 2.4(1) for the e(g)(t(2g)(+/-)), a(g)(t(2
g)(0)) and e'(g)(e(g)) orbitals respectively, the charge on the cobalt
ion being determined as +1.74(4). There is a large e(g)-e'(g) mixing
coefficient which leads to the conclusion that there is a significant
departure from the t(2g) octahedral character of the ground state orbi
tals. The results are consistent with a (4)A(g) ground state for the C
o2+ ion, which is in accord with the various earlier magnetic, spectro
scopic and heat capacity studies.