L. Mercier et C. Detellier, INTERCALATION OF TETRAALKYLAMMONIUM CATIONS INTO SMECTITES AND ITS APPLICATION TO INTERNAL SURFACE-AREA MEASUREMENTS, Clays and clay minerals, 42(1), 1994, pp. 71-76
Monolayer to bilayer (MTB) and bilayer to pseudotrimolecular (BTP) tra
nsitions were observed for smectites exchanged with symmetrical tetraa
lkylammonium cations of increasing sizes: +NR4, where R = (CH2)nCH3, w
ith 0 less-than-or-equal-to n less-than-or-equal-to 7. In the case of
SWy-1, SHCa-1 and SWa-1, the variation in layer spacing observed from
intercalation of tetramethylammonium up to tetraoctylammonium cations
showed a behavior characteristic of smectites with homogeneously distr
ibuted interlayer cations. In the case of STx-1, the change in interla
yer spacing with the increase of the alkyl chain length was characteri
stic of a very high charge heterogeneity. Higher charge smectites (SAz
-1 and SCa-3, CEC > 1.20 mmol/g) were found to have decreasing cation
exchange with increasing cation size, resulting in a ''leveling off''
of the interlayer spacing toward larger cations. The MTB and BTP trans
itions were used lo determine the internal surface area of various sme
ctites. The proposed method was found to be a quicker and simpler alte
rnative to the polar liquid sorption method for this measurement, but
was ineffective for high-charge smectites (CEC > 1.20 mmol/g).