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Isomorphously substituted zeolites

When applied to zeolites the term "isomorphous substitution" refers to the replacement of silicon or aluminum atoms by elements with ionic radii and coordination requirements which are compatible with the T (tetrahedral) sites of the zeolite structure. One method of preparing isomorphously substituted zeolites is to include a reactive source of the replacement... [Pg.374]

Details on the hydrothermal synthesis of FeMFI zeolites (with Fe-Al-Si and Fe-Si frameworks), and subsequent post-synthesis treatments have been described elsewhere. The isomorphously substituted zeolites were activated in steam (30vol.% H2O in 30 ml (STP) min of N2 flow) at two different temperatures (873 and 1173 K) during 5 h. Hereafter, the catalysts are denoted followed by the steam temperature, e.g. Fe-silicalite... [Pg.308]

An example of skeletal isomerization is the aldehyde/ketone rearrangement over zeolites (equation 3). Thereby the effects of variable acidity of isomorphous substituted zeolites and of shape selectivity on the course of the reaction are clearly evident [20]. [Pg.584]

It is the aim of the present paper to review the synthesis of a selected number of microporous materials which have more recently attracted the attention of zeolite scientists. The following selection criteria were appUed (i) the review is restricted to aluminosiUcates, hence, isomorphously substituted zeolites, SAPOs, MeAPOs and the Hke are not considered, (ii) crystalline microporous aluminosilicates are exclusively dealt with, the synthesis of ordered mesoporous molecular sieves (i.e. MCM-41) is not discussed and, (iii) especially those zeolites have been selected which, based on their particular structural or physicochemical properties, have a certain potential for appHcations in catalysis or adsorption. Some readers might miss such important and interesting zeolites like Beta, EMC-2, ZSM-12, etc. However, although there is still intensive research going on in the synthesis of these zeoHtes, their main synthesis principles have been summarized earUer [5,6] and will therefore not be discussed here. [Pg.66]

The isomorphic substituted aluminum atom within the zeolite framework has a negative charge that is compensated by a counterion. When the counterion is a proton, a Bronsted acid site is created. Moreover, framework oxygen atoms can give rise to weak Lewis base activity. Noble metal ions can be introduced by ion exchanging the cations after synthesis. Incorporation of metals like Ti, V, Fe, and Cr in the framework can provide the zeolite with activity for redox reactions. [Pg.213]

An extremely versatile catalyst for a variety of synthetically useful oxidations with aqueous hydrogen peroxide is obtained by isomorphous substitution of Si by Ti in molecular sieve materials such as silicalite (the all-silica analogue of zeolite ZSM-5) and zeolite beta. Titanium(IV) silicalite (TS-1), developed by Enichem (Notari, 1988), was the progenitor of this class of materials, which have become known as redox molecular sieves (Arends et al., 1997). [Pg.35]

Montmorillonite is a laminar and expandable clay with wet binding properties and widely available throughout the world. The layers have permanent negative charges due to isomorphic substitutions. The scientific interest of montmorillonite lies in its physical and chemical properties as well as its low price. Consequently, the industrial application of montmorillonite is an attractive process [1]. On the other hand, among numerous reports published so far, crystallization of zeolite Beta draws much attention because of its unique characteristics, in particular, acidity and acid catalysis. It is reasonable to conceive that a catalyst system based on Beta/montmorillonite composite with suitable composition should provide a good catalytic capacity. [Pg.137]

The catalyst samples were prepared in our laboratory. The synthesized Na-ZSM-5 zeolite was modified by conventional or solid state ion-exchange [11] to form H-, Fe-, Cu-, Ni- and Ti-ZSM5 samples, while the mesoporous catalysts (Fe- and Ti-MCM-41) were synthesized by isomorphous substitution [12], as well as the hydrotalcites containing Fe-, Cu-, Cr- or Ca-oxide in the Mg,Al-LDH structure [13]. [Pg.268]

The ZSM5 (Si/Al=40) as base zeolite was prepared by us. Cu was built in the framework by solid phase ion-exchange, Cr by conventional ion-exchange. Ni-samples were obtained by both methods. Ti-ZSM5 was synthesized by isomorphic substitution [8]. [Pg.438]

Macedo et al. [227] studied HY zeolites dealuminated by steaming, and found that the strength of intermediate sites decreased with increasing dealumination for Si/Al ratios varying from 8 to greater than 100. For comparison, isomorphously substituted HY, which is free of extra-framework cationic species, possesses more acid sites than conventionally dealuminated solids with a similar framework Si/Al ratio [227], This is because some of the extra-framework aluminum species act as charge-compensating cations and therefore decrease the number of potential acid sites. [Pg.243]

Extensive studies of the acidity and basicity of zeolites by adsorption calorimetry have been carried out over the past decades, and many reviews have been published [62,64,103,118,120,121,145,146,153,154]. For a given zeolite, different factors can modify its acidity and acid strength the size and strength of the probe molecule, the adsorption temperature, the morphology and crystallinity, the synthesis mode, the effect of pretreatment, the effect of the proton exchange level, the Si/Al ratio and dealumination, the isomorphous substitution, chemical modifications, aging, and coke deposits. [Pg.243]

Changes In shape selectivity due to the Isomorphous substitution of A1 by the larger Fe has not, so far, been unequivocally been established. However, differences in catalytic activity, selectivity and stability between alumino- and ferrisillcate zeolites arising from the presence of weaker... [Pg.50]

A unique titanium(IV)-silica catalyst prepared by impregnating silica with TiCLt or organotitanium compounds exhibits excellent properties with selectivities comparable to the best homogeneous molybdenum catalysts.285 The new zeolite-like catalyst titanium silicalite (TS-1) featuring isomorphous substitution of Si(IV) with Ti(IV) is a very efficient heterogeneous catalyst for selective oxidations with H2C>2.184,185 It exhibits remarkable activities and selectivities in epoxidation of simple olefins.188,304-306 Propylene, for instance, was epoxidized304 with 97% selectivity at 90% conversion at 40°C. Shape-selective epoxidation of 1- and 2-hexenes was observed with this system that failed to catalyze the transformation of cyclohexene.306 Surface peroxotitanate 13 is suggested to be the active spe-... [Pg.457]

Difluorobenzenes are isomerized under gas-phase conditions in the presence of metallosilicates, containing the structure of pentasil zeolites with isomorphic substitution of some silicon atoms by aluminum, gallium, or iron.4 A German patent describes the isomerization of l-bromo-2,4-difluorobenzene to l-bromo-3,5-difluorobenzene in pentasil-type zeolites in an autoclave at 320 C and 25 x 105 Pa for 1 h, giving 29% conversion and 73% selectivity.5... [Pg.232]

From a mechanistic viewpoint it is worth noting that the TS-1 catalyst contains the same chemical elements in roughly the same proportions as the Shell amorphous TiIV/Si02 catalyst referred to earlier. However, the former displays a much broader range of activities than the latter. A possible explanation may be that the TS-1 catalyst contains more (or more active) isolated titanyl centres than the amorphous Ti1v/Si02. Based on the quite remarkable results obtained with TS-1 we expect many more examples of redox zeolites, i.e. zeolites, alpos, etc. modified by isomorphous substitution with redox metal ions in the crystal lattice, as selective oxidation catalysts.66... [Pg.50]

The synthesis of these titanium-substituted zeolites has been described to occur by a secondary synthesis process involving the reaction of [NH4]2TiF6 with the preformed corresponding zeolite (Section IV.G). The chemical and physicochemical properties described are not sufficient to establish the presence of Tiiv ions in framework positions. The titanium concentrations reported are much higher than the maximum values observed in titanium silicates for which isomorphous substitution has been demonstrated. The possible presence of Ti02 particles has not been investigated. No indication of the properties of these materials as catalysts in reactions typical of titanium silicates has been provided. It is therefore very doubtful that real isomorphous substitution has been obtained (Skeels et al., 1989 Skeels, 1993). [Pg.287]

Most zeolites have an intrinsic ability to exchange cations [1], This exchange ability is a result of isomorphous substitution of a cation of trivalent (mostly Al) or lower charges for Si as a tetravalent framework cation. As a consequence of this substitution, a net negative charge develops on the framework of the zeolite, which is to be neutralized by cations present within the channels or cages that constitute the microporous part of the crystalline zeolite. These cations may be any of the metals, metal complexes or alkylammonium cations. If these cations are transition metals with redox properties they can act as active sites for oxidation reactions. [Pg.125]

The other way to introduce heterometals is their isomorphous substitution for Si in the framework, in a similar manner to the isomorphous substitution of Al. The heteroatoms should be tetrahedral (T) atoms. In hydrothermal synthesis, the type and amount of T atom, other than Si, that may be incorporated into the zeolite framework are restricted due to solubility and specific chemical behavior of the T-atom precursors in the synthesis mixture. Breck has reviewed the early literature where Ga, P and Ge ions were potentially incorporated into a few zeolite structures via a primary synthesis route [9]. However, until the late 1970s, exchangeable cations and other extraframework species had been the primary focus of researchers. [Pg.126]


See other pages where Isomorphously substituted zeolites is mentioned: [Pg.375]    [Pg.382]    [Pg.1164]    [Pg.375]    [Pg.382]    [Pg.1164]    [Pg.329]    [Pg.52]    [Pg.113]    [Pg.116]    [Pg.28]    [Pg.40]    [Pg.9]    [Pg.235]    [Pg.422]    [Pg.43]    [Pg.344]    [Pg.357]    [Pg.32]    [Pg.522]    [Pg.117]    [Pg.169]    [Pg.327]    [Pg.356]    [Pg.199]    [Pg.244]    [Pg.282]    [Pg.282]    [Pg.287]    [Pg.126]    [Pg.129]    [Pg.135]   


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Isomorphic

Isomorphism

Isomorphism substitution

Isomorphous

Isomorphs

Substitutional isomorphism

Zeolites isomorphous substitution

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