Bentonite and illite were interacted with nonyl- and dodecylammonium salt s
olutions to see how the alkylammonium ions became attached and oriented wit
hin the interlamellar space of the clays. X-ray diffraction analyses were c
arried out to obtain information on the interlamellar organization and orie
ntation of the adsorbed alkylammonium compounds. Thermogravimetric analysis
(TG, DTG) and Fourier Transform Infrared Analyses (FTIR) were performed to
characterize the samples and to determine the amounts adsorbed by the clay
samples. The modification process was effective in nonyl- and dodecylammon
ium bentonites. Alkylammonium ions were adsorbed in the interlamellar space
of the clays. Regarding the orientation of the alkylammonium ions between
the silicate sheets, it was found that the organic cation alkylchains were
parallel to the silicate layer. Intercalation was generally greater with DA
ions.