The mechanism of-formation of carbonaceous deposits on montmorillonites was
studied for systems prepared by sorption of polymers on pillared-montmoril
lonites and subsequent carbonization. Temperature-programmed desorption of
ammonia and X-ray photoelectron spectroscopy showed that polymer was attach
ed to Al-OH acidic sites of smectite layers. Pillars were not influenced to
a greater extent. Islands of carbonaceous material were formed, but the am
ount of deposited carbon depended strongly upon carbonization conditions. T
he hydrophylic and acidic properties of carbon-covered silica aluminas diff
ered strongly from those of the Starting material. (C) 2000 Academic Press.