B. Sulikowski, ISOMORPHOUS REPLACEMENT IN THE ZEOLITIC FRAMEWORKS - RECENT ADVANCES AND IMPLICATIONS, Heterogeneous chemistry reviews, 3(3), 1996, pp. 203-268
Citations number
487
Categorie Soggetti
Chemistry Physical","Physics, Atomic, Molecular & Chemical
Isomorphous substitution in zeolites by silicon, aluminium, boron, gal
lium, germanium, titanium, vanadium and iron is described. Since the c
atalytic properties of the solid are inextricably linked to its struct
ure and composition, much effort has been devoted in recent years to p
reparing zeolitic materials containing heteroatoms in their framework.
The consequences of substitution of heteroatoms into 'regular' crysta
lline aluminosilicates are described, including methods of preparation
and properties of these novel materials. The theoretical basis of rep
lacement is first dealt with. The experimental progress made in charac
terization of molecular sieves is exemplified by extensive use of MMR,
EXAFS, neutron scattering and laser Raman spectroscopy data, in addit
ion to other techniques. In particular, the short-range order of Si an
d X (where X = Al or other heteroatom) located in the zeolitic framewo
rk has been explored by solid-state NMR. This turned out to be a key m
ethod in understanding the properties of dealuminated and recently obt
ained reilluminated zeolites. Fractals, at first a purely mathematical
concept, have found multiple applications in chemistry and materials
science. Here we present how the fractal dimension of dealuminated and
realuminated faujasites can be measured. The results are interpreted
satisfactorily within the frame of XRD, FT IR and MAS NMR studies of t
hose solids. Finally, the catalytic behaviour of metallosilicates, in
both gas phase and Liquid phase, is discussed. It is shown that in add
ition to acidic catalysts, redox-type zeolite catalysts can be success
fully prepared (e.g. gallium-, titanium- and vanadosilicates). Such so
lids can be used in a number of oxidation and reduction reactions. Tak
ing into account the progress made in understanding isomorphous substi
tution in zeolites, there is no doubt that many novel and surprising m
aterials will be synthesized in the future.