Thermal desorption-degradation of cyclohexylamine over Ni2+- and Al3+-exchanged bentonite studied using evolved gas analysis (TG-EGA) and diffuse reflectance spectroscopy (DRIFTS)

Ni2+- and Al3+-exchanged montmorillonite are known to demonstrate Lewis and Bronsted acidity, respectively, when probed using the diagnostic base pyri dine (C. Breen, Clay Miner., 1991, 26, 487). Thermogravimetric analysis (TG A) of pyridine saturated Al3+- and Ni2+-montmorillonite differ whereas here it was found that cyclohexylamine (CHA) desorption profiles were very simi lar, albeit CHA was held to a higher temperature on Ni2+-SWy-2 than on Al3-SWy-2. Evolved gas analysis (EGA) of the desorbed products revealed signif icant differences in the amount of cyclohexylamine, cyclohexene, methylcycl opentene, benzene and aniline produced, which demonstrated different decomp osition pathways for CHA sorbed to Al3+- and Ni2+-exchanged SWy-2. For exam ple, cyclohexene is produced over both exchange forms whereas aniline and m ethylcyclopentene were the major products over Ni2+- and Al3+-SWy-2, respec tively. Variable-temperature DRIFTS was unable to distinguish between CHA-t reated Al3+- and Ni2+-SWy-2 at temperatures < 250 degrees C, but at 300 deg rees C the Ni2+ form exhibited a strong, intense band at 1648 cm(-1) which identifies cyclohexylimine as a surface bound intermediate which transforms before desorption.