The dehydroxylation of boehmite has been studied by the application of infrared emission spectroscopy over the 200 to 750 degrees C temperature range. The dehydroxylation is followed by the loss of intensity of the hydroxyl stretching frequencies observed at 3478, 3319, and 3129 cm(-1) and by the loss of intensity of the hydroxyl deformation modes at 1140 and 1057 cm(-1). Dehydroxylation starts at 250 degrees C and is complete by 450 degrees C. No difference was found between the synthetic and natural boehmite dehydroxylation. The hydroxyl stretching frequencies show a pronounced blue shift, while the hydroxyl deformation modes show a pronounced red shift. Infrared absorption bands were observed at 3413, 3283, and 3096 cm(-1) for the hydroxyl stretching frequencies and at 1161 and 1071 cm-L for the hydroxyl deformation frequencies. Low-frequency infrared absorption bands are observed at 749, 635, and 542 cm(-1) and infrared emission bands at 811, 716, 611, and 456 cm(-1). The infrared emission low-frequency bands moved to higher frequencies upon thermal treatment. Spectral changes in the low-frequency bands confirm that dehydroxylation commenced at 250 degrees C. Infrared emission spectroscopy allows the phase changes of the Al2O3-H2O alumina system to be studied irt situ at the elevated temperatures.