J. Madejova et al., PREPARATION AND INFRARED SPECTROSCOPIC CHARACTERIZATION OF REDUCED-CHARGE MONTMORILLONITE WITH VARIOUS LI CONTENTS, Clay Minerals, 31(2), 1996, pp. 233-241
A series of reduced-charge montmorillonites (RCMs) was prepared from L
i-montmorillonite from Jelsovy Potok (Slovakia) by heating at various
temperatures (105-210 degrees C) for 24 h. The amount of fixed Li, 0.0
9-0.67 per O-20(OH)(4), increased with increasing temperature, confirm
ing preparation of a set of samples of variable layer charge from the
same parent Li-montmorillonite by varying only the preparation tempera
ture. Infrared spectroscopy revealed that Li was trapped in the hexago
nal cavities of the tetrahedral sheet at all temperatures. Partial dep
rotonation of the samples, reflected in the decrease of the intensitie
s of the OH-bending bands, was observed after treatments above 120 deg
rees C. Analysis of the OH-stretching region showed Li in the previous
ly vacant octahedra in the samples heated above 150 degrees C. Weak in
flections near 660 and 720 cm-L confirmed development of local triocta
hedral character of octahedral cations coordinated with OH groups in t
he sample heated at 210 degrees C. Gradual decrease of the layer charg
e, due to Li fixation led to a shift of the Si-O stretching band to hi
gher frequencies and to the appearance of new, pyrophyllite-like bands
at 1120 and 419 cm(-1).