198 Topics in Current Chemistry Editorial Board: A. de Meijere KN ...
198 Topics in Current Chemistry Editorial Board: A. de Meijere KN ...
198 Topics in Current Chemistry Editorial Board: A. de Meijere KN ...
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132 Y. Aoyama<br />
4 Catalysis . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 154<br />
4.1 Criteria of Zeolitic Catalysis . . . . . . . . . . . . . . . . . . . . . . . 154<br />
4.2 Catalysis by a Hydrogen-Bon<strong>de</strong>d Organic Solid . . . . . . . . . . . . 154<br />
4.3 Immobilization ofSoluble Metal Complexes . . . . . . . . . . . . . . 157<br />
5 Conclud<strong>in</strong>g Remarks and Future Prospects . . . . . . . . . . . . . . 158<br />
5.1 Manipulation of Pores . . . . . . . . . . . . . . . . . . . . . . . . . . 158<br />
5.2 Solid Catalysts <strong>in</strong> Organic Transformations . . . . . . . . . . . . . . 158<br />
5.3 Organic Zeolite Analogues as Enzyme Mimics <strong>in</strong> Water . . . . . . . 159<br />
6 References . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 159<br />
1<br />
Introduction<br />
Zeolites are a class of microporous <strong>in</strong>organic crystals composed of alum<strong>in</strong>osilicate<br />
tetrahedra, whose <strong>in</strong>ternal cavities are capable of not only reversible guest<br />
b<strong>in</strong>d<strong>in</strong>g but also catalys<strong>in</strong>g chemical reactions [1–5]. These unique properties<br />
challenge chemists to mimic some of the zeolitic functions by us<strong>in</strong>g organic or<br />
metal-organic components [6–9]. A great advantage of molecular solid materials<br />
is that they are spontaneously formed from molecular build<strong>in</strong>g blocks. The<br />
diversity and <strong>de</strong>signability of organic structures as well as <strong>in</strong>termolecular <strong>in</strong>teractions<br />
spur the research activity <strong>in</strong> this area [10–13].<br />
There is no wi<strong>de</strong>ly-accepted <strong>de</strong>f<strong>in</strong>ition of organic zeolite analogues. The <strong>de</strong>f<strong>in</strong>ition<br />
may <strong>de</strong>pend on the functions expected for such materials. An obvious<br />
function is as selective adsorbents, which may be used <strong>in</strong> the separation, purification,<br />
or trapp<strong>in</strong>g and storage of particular chemicals [6, 9]. Another potential<br />
one is that of functional materials as either host-guest adducts or guest-free<br />
porous solids, which may exhibit unique electronic, optical or mechanical<br />
properties [14, 15]. Still, a third or a most important function is that of solid<br />
catalysts, which should be readily recovered; this is highly attractive from the<br />
environmental as well as resource utilisation viewpo<strong>in</strong>ts. In mimick<strong>in</strong>g the key<br />
guest-b<strong>in</strong>d<strong>in</strong>g properties of zeolites, a variety of lattice <strong>in</strong>clusion compounds<br />
were prepared, where guest molecules were <strong>in</strong>clu<strong>de</strong>d <strong>in</strong> well-<strong>de</strong>f<strong>in</strong>ed host cavities<br />
[6–13]. However,“unusual” properties and catalytic activities of solid organic<br />
hosts rema<strong>in</strong> almost completely unexplored. Heterogeneous catalysts have so<br />
far been exclusively <strong>in</strong>organic materials <strong>in</strong>clud<strong>in</strong>g zeolites. In addition to the<br />
general problems <strong>in</strong> crystal eng<strong>in</strong>eer<strong>in</strong>g [16, 17], there seem to be a couple of<br />
fundamental questions associated with functional organic zeolite analogues.<br />
One is static or structural; is it really possible to ma<strong>in</strong>ta<strong>in</strong> a large volume of<br />
permanent voids <strong>in</strong> the absence of any guests <strong>in</strong> organic crystals? The other is<br />
dynamic or k<strong>in</strong>etic; how do molecules diffuse <strong>in</strong> solid materials?<br />
The object of this article is to review the present stage of mimick<strong>in</strong>g the zeolitic<br />
functions, to highlight the achievement, although very prelim<strong>in</strong>ary, <strong>in</strong> construct<strong>in</strong>g<br />
catalytic organic and metal-organic solids, and to discuss the problems