M. Wildner, POLARIZED ELECTRONIC ABSORPTION-SPECTRA OF CO2-TYPE COMPOUNDS COSO4-CENTER-DOT-H2O AND COSEO4-CENTER-DOT-H2O( IONS IN THE KIESERITE), Physics and chemistry of minerals, 23(8), 1996, pp. 489-496
Polarized electronic absorption spectra of the kieserite-type compound
s CoSO4 . H2O and CoSeO4 . H2O have been obtained at room temperature
(spectral range 35000-5000 cm(-1)) and at liquid nitrogen temperature
(visible spectral region), using microscope-spectrometric techniques.
The spectra are interpreted and evaluated in terms of a tetragonal cry
stal field formalism for the d(7) configuration, in regard to the pseu
dotetragonal elongation of the CoO4(H2O)(2) octahedra, known from prev
ious X-ray structure investigations, employing the tetragonal paramete
rs Dq, Dt, and Ds, and the Racah parameters B and C. The observed and
calculated energy levels are in good agreement for the following param
eter sets: CoSO4 . H2O: Dq=826, Dt=40, Ds=350, B=856, C=3580 cm(-1); C
oSeO4 . H2O: Dq=817, Dt=44, Ds=406, B=841, C=3490 cm(-1); correspondin
g 'cubic' crystal field strengths Dq(cub) are 803 and 792 cm(-1), resp
ectively. The values of Dq((cub)), Racah B and C are in the common ran
ge for Co2+ ions in (pseudo)octahedral fields of oxygen ligands, and t
heir differences in CoSO4 . H2O compared to CoSeO4 . H2O are consisten
t with somewhat different mean Co-O bond lengths and with a slightly h
igher covalent contribution to Co-O bonding in the selenate compound.
The values found for the parameter Dt, which is directly correlated to
the extent of tetragonal distortion, are much lower than expected fro
m purely geometrical considerations, thus confirming a significantly h
igher position of H2O ligands in the spectrochemical series compared t
o oxygen ligands belongingto SO4 or SeO4 groups.