焦炭
催化作用
甲醇
化学
膨润土
化学工程
介孔材料
沉积(地质)
材料科学
有机化学
沉积物
古生物学
工程类
生物
作者
Andrés T. Aguayo,Ana E. Sánchez del Campo,Ana G. Gayubo,Ana M Tarrío,Javier Bilbao
标识
DOI:10.1002/(sici)1097-4660(199904)74:4<315::aid-jctb34>3.0.co;2-g
摘要
When methanol is converted to olefins on a SAPO-34 catalyst between 350 and 425°C, there is a rapid initial formation of coke, followed by a slower rate of coke deposition. The rate of coke formation decreases with increasing temperature, and with progression through the catalyst bed. The coke completely blocks the internal channels of the SAPO-34 crystals and subsequently blocks the mesopores (intercrystalline and those of the bentonite). Coke deposition mainly blocks sites of acidic strength above 175 kJ mol−1. The presence of water in the feed lessens coke formation, either by converting Lewis to Brønsted sites or by competing for surface sites with coke precursors. © 1999 Society of Chemical Industry
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