“…On the other hand, high temperature peaks could be associated to the presence of chemical interactions that may lead to oligomer cracking. Oligomer formation is associated with hydroxyl groups attached to the surface of the zeolite that provide sites for aliphatic carbon adsorption that may ultimately lead to oligomerisation [26]. Then, a similar interpretation could be carried out in the case of ZSM-5 and SAPO-41, where several peaks can be identified.…”
Section: Temperature Programme Desorption Profilesmentioning
“…On the other hand, high temperature peaks could be associated to the presence of chemical interactions that may lead to oligomer cracking. Oligomer formation is associated with hydroxyl groups attached to the surface of the zeolite that provide sites for aliphatic carbon adsorption that may ultimately lead to oligomerisation [26]. Then, a similar interpretation could be carried out in the case of ZSM-5 and SAPO-41, where several peaks can be identified.…”
Section: Temperature Programme Desorption Profilesmentioning
“…We note, however, there is no reliable method for identifying the Brønsted acid strength, which is essential for the activation of the reactants and further catalyzed reactions in these 8-ring zeolites. Presently, the acid strength can only be estimated by the theoretical modeling [24]. Nevertheless, the poor catalytic performance of H/MTF zeolits upon ethylene transformation indicates that H/MTF might have weaker acidities than H/MFI.…”
Section: Ethanol and Ethylene Transformations On The Catalystsmentioning
Aluminosilicate H/CHA and H/MTF zeolites show remarkably different catalytic activities in the methanol and ethanol transformations although they have similar pore size of 8-membered ring structures. Moreover, the produced ethylene is further converted on H/CHA, but H/MTF is not active for the ethylene transformation. The correlations between the distinct catalytic differences and their intrinsic structural properties, including topology and acidity, are discussed.
“…Most of these species diffuse slowly in the zeolite pores. It must also be kept in mind that the physisorbed alkenes are most likely in equilibrium with the corresponding alkoxy species formed by reaction with the Brønsted acid sites (25), although no direct IR evidence of this equilibrium was obtained in the current study.…”
Section: On the Nature Of The Sorbed Species In H-fermentioning
confidence: 66%
“…The direct evidence for the formation of the alkoxide was not available, because the spectral region below 1200 cm −1 , where ν C-O can be observed (24), was not accessible. Carbenium ions in thermal equilibrium with the alkoxide and butene species may also be present (25); however, the main IR absorption feature of these compounds (CCC asym. stretch at ca.…”
Section: But-1-ene Reactions At Different Temperaturesmentioning
The sorption and reaction of but-1-ene over a ferrierite sample was studied by in situ IR spectroscopy to relate the selectivity to isobutene and the sorbed species. The spectra highlighted the presence of various unsaturated species including polyenes, which were readily formed upon contacting H-FER with but-1-ene while a poor selectivity to isobutene was observed. Aromatic compounds were concluded to be subsequently formed via dehydrogenation/cyclization of the polyenic deposits while the isobutene selectivity increased via suppression of by-products. These data support earlier assumptions that the initial high yield of by-products was produced by the reaction of butenes with reactive deposits, which were gradually converted into more inert aromatic deposits. Upon purging the catalyst with an inert, branched C 8 hydrocarbons and aromatic molecules such as xylenes desorbed. The rates of desorption showed an initially linear variation with the square root of time and were fitted to a monodimensional Fickian model. Because the slowly diffusing species were rather abundant during the course of the reaction, it is proposed that the skeletal isomerization was effectively limited to the acid sites close the pore mouth of H-FER crystallites. c 2002 Elsevier Science (USA)
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