2014
DOI: 10.1016/j.cattod.2014.03.023
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Bioethanol conversion into hydrocarbons on HZSM-5 and HMCM-22 zeolites: Use of in situ DRIFTS to elucidate the role of the acidity and of the pore structure over the coke formation and product distribution

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Cited by 42 publications
(58 citation statements)
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“…This is accompanied by a change in the 3000 to 2880 cm -1 region where the intensity of the peaks at 2903 and 2875 cm -1 decrease as the signal at 2938 cm -1 increases. [24,29] As these signals are still present above 200 o C, they are attributed to the chemisorbed ethoxy species. This is likely due to a decrease in all four of the ethanol peaks (2982, 2938, 2903 and 2875 cm -1 ), and an increase in the ethoxy signal (2938 and 2982 cm 1 ).…”
Section: Resultsmentioning
confidence: 99%
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“…This is accompanied by a change in the 3000 to 2880 cm -1 region where the intensity of the peaks at 2903 and 2875 cm -1 decrease as the signal at 2938 cm -1 increases. [24,29] As these signals are still present above 200 o C, they are attributed to the chemisorbed ethoxy species. This is likely due to a decrease in all four of the ethanol peaks (2982, 2938, 2903 and 2875 cm -1 ), and an increase in the ethoxy signal (2938 and 2982 cm 1 ).…”
Section: Resultsmentioning
confidence: 99%
“…[29] This last observation suggests that is commonly attributed to methyl rocking of C-C-O-C-C species, which suggests the early (low temperature) formation of diethyl ether species. [24,25,30] It is noted that other bands may also be attributed to diethyl ether, though these bands (2982, 2875, 1485, 1450 and 1395 cm -1 ) typically overlap with ethanol and the ethoxy species. [24,25,30] The appearance of diethyl ether at low temperature is partly attributed to the strong acid sites present on SAPO-34, and also due to the energetic incentive of forming diethyl ether (-42 kJ/mol).…”
Section: Resultsmentioning
confidence: 99%
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