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Zeolites cyclopentenyl cations

The resultant cycloalkenyl carbenium ions, especially the cyclopentenyl cations, are very stable (103,104) and can even be observed as free cations in zeolites 105,106). These ions can oligomerize further and, within zeolites, irreversibly block the acidic hydroxyl groups. With liquid acids, the oligomers will dilute the acid and thus lower its acid strength. [Pg.274]

Propene on HY was, therefore, selected for the first in situ variable-temperature study using the CAVERN method. These experiments were carried out in early 1988 and published in 1989 (93). The central features of the CAVERN experiments were that the propene was introduced into the zeolite at cryogenic temperature and the sample was manipulated so that spectral acquisition could commence with an unreacted sample. Additional spectra were then acquired as the sample was slowly raised to room temperature. Detailed experiments of this sort were carried out for propene-2-l3C and propene-7-13C and less extensive experiments were performed for propene-3-13C. These experiments showed, among other things, that the 250 ppm peak was formed coincident with a second peak at ca. 156 ppm and the relative intensities of these peaks were 2 1. A careful study of the literature of carbenium ion chemistry in sulfuric acid and superacid solution media suggested the assignment of these resonances (250 and 156 ppm) to alkyl-substituted cyclopentenyl cations similar to 4. [Pg.141]

Fig. 12. 75.4-MHz 13C CP/MAS spectra showing the formation of cyclopentenyl cations 8 from cycIopentene-13Ci (random) on zeolite HZSM-5 and 4 from propene-2-,3C on zeolite UY. Fig. 12. 75.4-MHz 13C CP/MAS spectra showing the formation of cyclopentenyl cations 8 from cycIopentene-13Ci (random) on zeolite HZSM-5 and 4 from propene-2-,3C on zeolite UY.
The principal components of the trityl cation in zeolite HY are <5 = 282 ppm and <5j = 55 ppm. It is instructive to tabulate all of the 13C principal component data measured for free carbenium ions in zeolites as well as for a few carbenium ions characterized in other solid acid media (Table III). The zeolitic species, in addition to the trityl cation (119), are the substituted cyclopentenyl cation 8 (102), the phenylindanyl cation 13, and the methylindanyl cation 12 (113). Values for the rert-butyl cation 2 and methylcyclopentyl cation 17 (prepared on metal halides) (43, 45) are included for comparison. Note that the ordering of isotropic chemical shifts is reasonably consistent with one s intuition from resonance structures i.e., the more delocalized the positive charge, the smaller the isotropic shift. This effect is even more apparent in the magnitudes of the CSA. Since... [Pg.149]

CP/MAS NMR identification of isopropoxide as an intermediate in propylene-2- C conversion on zeolite HY. The signals at 150 and 250 ppm are due to the cyclopentenyl cations also formed under reaction conditions [15]. Here denotes the C-label in propylene. [Pg.167]


See other pages where Zeolites cyclopentenyl cations is mentioned: [Pg.264]    [Pg.32]    [Pg.93]    [Pg.155]    [Pg.157]    [Pg.404]   
See also in sourсe #XX -- [ Pg.42 , Pg.140 , Pg.141 , Pg.142 ]

See also in sourсe #XX -- [ Pg.140 , Pg.141 , Pg.142 ]




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