In order to assess the influence of tetrahedral sheet charge on the hydroxy
l-stretching vibration in clay minerals, a series of synthetic Na saponites
, with increasing layer charge, was studied by infrared (IR) spectroscopy.
When recorded after KBr dilution either in transmission or diffuse reflecta
nce, the IR spectra exhibit a component at similar to 3710 cm(-1), the inte
nsity of which increases linearly with increasing layer charge. When experi
ments are carried out without any dilution of the samples, this component i
s not observed, suggesting a Na+/K+ exchange upon mixing of the sample with
KBr. The spectra obtained for K-saponite confirm this exchange. This shows
that the dilution procedure can lead to serious misinterpretations of IR s
pectra in the OH-stretching region.