The Mossbauer and infrared spectra of Li- and Rb-saturated nontronites from
Washington, USA (SWa-1), heat treated at different temperatures, were meas
ured. The Mossbauer results show that diffusion of Li+ into the 2:1 layer b
y heat treatment at 250-300 degrees C does nor affect the magnetic hyperfin
e interactions of the octahedral iron centers. In contrast, significant cha
nges were observed by calcination at temperatures >300 degrees C for Li-sat
urated nontronites. The main features of the Mossbauer spectra recorded at
different temperatures reveal superparamagnetic behavior with a blocking te
mperature of similar to 5 K. The superparamagnetic behavior is related to s
mall magnetic domains created by partially broken Fe-O-Fe bonds upon hear t
reatment. The infrared spectra of Li-rich nontronite, heat treated at 300 d
egrees C, show changes attributed to Li migration into the hexagonal caviti
es. Heating to higher temperatures, produced changes in the spectra of the
Li- and Rb-saturated nontronites owing to the dehydroxylation of the layer
structure. The dehydroxylation process begins with the loss of OH groups in
the FeOHFe bridges and is completed with the disruption of the Al-O bonds
at >600 degrees C.