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Titanosilicate zeolites

Zeolite structures typically consist of silicon and aluminum finked by tetrahedrally coordinating oxygen atoms. However, similar structures as found for these aluminosilicates can be formed by substitution of the aluminum by other elements (e.g., Ga in gallosilicates or Ti in titanosilicates). Even the substitution of both Si and A1 is possible, as for example in aluminophosphates or... [Pg.99]

Since titanosilicates generally require specific synthesis conditions in comparison to silicalites and aluminosilicates, many efforts made to synthesize those of numerous zeolite structures have led to a very limited success. This has also been the case with the MWW zeolite. Although it is possible to hydrothermally synthesize MWW... [Pg.137]

The use of heterogeneous catalysts in the synthesis of urethanes from aliphatic and aromatic amines, C02 and alkyl halides has been explored only recently. Titanosilicate molecular sieves [60a], metal phthalocyanine complexes encapsulated in zeolite-Y [60a], beta-zeolites and mesoporous silica (MCM-41) containing ammonium cations as the templates [60b, c], and adenine-modified Ti-SBA-15 [60d, e] each function as effective catalysts, even without any additional base. [Pg.131]

The first materials discovered which belong to this novel group of titanosilicates, having numerous sixfold-coordinated Ti sites in a microporous crystalline array, was ETS-4, which is an analogue of the mineral zorite while the other, ETS-10, is topologically comparable to zeolite (1 [96],... [Pg.366]

An ideal approach to achieving chiral induction in a constrained medium such as zeolite would be to make use of a chiral medium. No zeolite that can accommodate organic molecules, currently exists in a stable chiral form. Though zeolite beta and titanosilicate ETS-10 have unstable chiral polymorphs, no pure enantiomorphous forms have been isolated. Although many other zeolites can, theoretically, exist in chiral forms (e.g., ZSM-5 and ZSM-11) none has been isolated in such a state. In the absence of readily available chiral zeolites, one is left with the choice of creating an asymmetric environment within zeolites by the adsorption of chiral organic molecules. [Pg.605]


See other pages where Titanosilicate zeolites is mentioned: [Pg.193]    [Pg.27]    [Pg.457]    [Pg.151]    [Pg.27]    [Pg.13]    [Pg.57]    [Pg.193]    [Pg.27]    [Pg.457]    [Pg.151]    [Pg.27]    [Pg.13]    [Pg.57]    [Pg.36]    [Pg.45]    [Pg.8]    [Pg.190]    [Pg.142]    [Pg.194]    [Pg.418]    [Pg.77]    [Pg.78]    [Pg.418]    [Pg.418]    [Pg.126]    [Pg.136]    [Pg.143]    [Pg.145]    [Pg.150]    [Pg.209]    [Pg.40]    [Pg.82]    [Pg.366]    [Pg.184]    [Pg.572]    [Pg.258]    [Pg.142]    [Pg.1]    [Pg.246]    [Pg.324]    [Pg.170]    [Pg.278]    [Pg.28]   
See also in sourсe #XX -- [ Pg.151 ]

See also in sourсe #XX -- [ Pg.151 ]




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Titanosilicate

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