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Introduction to Nanotechnology

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276 SELF-ASSEMBLY AND CATALYSIS<br />

Figure 10.19. Sketch of the structure of the (A10,[Al(OH)2H20],,)7+ Keggin ion with one<br />

tetrahedral group A104 in the center position of Fig. 10.18, surrounded by 12 A106 octahedra<br />

at the remaining sites of Fig. 10.18, where the oxygens 0; of the octahedra belong <strong>to</strong> hydroxyl<br />

groups OH, or <strong>to</strong> water molecules H20. [From A. Clearfield, in Moser (1996), Chapter 14, p. 348.1<br />

of the silicate layers in 6.5 unit cells, the distance between nearest-neighbor pillars<br />

can be estimated. If the pillars are assumed <strong>to</strong> form a square lattice, then the spacing<br />

between the center points of nearest-neighbor pillars is (A)'/' = 1.77 nm, and if they<br />

are arranged on a regular triangular or hexagonal lattice, then their separation is<br />

(2A/1/5)'l2 = 1.9Onm. Taking an average of these two values, one obtains a free<br />

space of about 0.74 nm between pillars. Experimental measurements indicate that<br />

the resulting pillared clay has a basal spacing of "1.85 tun, a surface area of<br />

E 250 m2/g, and a pore volume of -0.2 cm3/g.<br />

One important aspect of pillared clays that contributes <strong>to</strong> their catalytic properties<br />

is the presence of acid sites, which can be of the Lewis or Brransted types, as<br />

explained in the previous section. When a pill'ared clay is heated the water and<br />

hydroxyl groups split out pro<strong>to</strong>ns <strong>to</strong> balance the negative charges of the layers as the<br />

pillars approach electrical neutrality, and this generates considerable Brransted<br />

acidity. Lewis acid sites are generated on the layers by defect formation, and on<br />

the pillars by dehydroxylation, or the removal of OH groups. To confirm the<br />

presence of these sites on the PILC surface, the heterocyclic ring compound pyridine<br />

(C,H,N) was adsorbed and an infrared spectrum was recorded. This spectrum<br />

exhibited a strong IR band at 1453 cm-l arising from Lewis acid sites, and a weaker<br />

band at 1550 cm-I produced by Brransted sites.<br />

The discussion until now has centered around the clay saponite pillared by the<br />

Keggin ion. Other types of montmorillonite clay materials have been used and other<br />

metal oxide polymers have served as pillars. Examples of nonalumina pillars are

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