勃姆石
红外线的
红外光谱学
化学
光谱学
分析化学(期刊)
傅里叶变换红外光谱
吸收(声学)
铝
光化学
材料科学
光学
有机化学
复合材料
量子力学
物理
作者
Ray L. Frost,J. Theo Kloprogge,Shane C. Russell,Jennifer Szetu
标识
DOI:10.1366/0003702991946938
摘要
The dehydroxylation of boehmite has been studied by the application of infrared emission spectroscopy over the 200 to 750 °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 °C and is complete by 450 °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 −1 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°C. Infrared emission spectroscopy allows the phase changes of the Al 2 O 3 –H 2 O alumina system to be studied in situ at the elevated temperatures.
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