Silica gel monoliths containing Co2+ with a Co/Si molar ratio up to 1/
20 were prepared by acid-catalyzed hydrolysis of tetraethoxysilane in
the presence of cobalt nitrate and formamide. UV-visible spectra recor
ded at different steps of the preparation showed important changes in
the Co2+ environment. A change from octahedral to tetrahedral environm
ent was observed during aging. It was attributed to the formation of b
onds between cobalt ions and the gel skeleton induced by an increase o
f pH. In xerogels, Co2+ was in tetrahedral coordination and the calcin
ation temperature in the 300 to 700 degrees C range had no influence o
n the spectra. A partial reverse evolution from tetrahedral to octahed
ral was observed when calcinated gels were exposed to moisture.