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Structured packing, dehydration

When these minerals are heated they dehydrate in a remarkable way by extruding little wormlike structures as indicated by their name (Latin vermiculus, little worm) the resulting porous light-weight mass is much used for packing and insulation. The relationship between the various layer silicates is summarized with idealized formulae in Table 9.10 (on page 357). [Pg.354]

Of interest here is the question relating to the value for the slope coefficient, k, from equation (1), when surfactant structures incorporating both ionic (say sulphonate) and nonionic moieties are included together. The Ghanges in electric double layer effects imparted from salt addition might dominate the packing constraints and therefore the phase inversion process, or perhaps oxyethylene dehydration effects from the presence of toluene could also play a role. [Pg.323]

Thus-formed SAM s are densely packed, ordered films, attached to the surface with chemical bonds. Alkyl chains are aligned paralel in a densely packed fashion. The surface is fully covered, irrespective of the number of hydroxyl groups. Not all silane molecules are covalently linked to the surface. Le Grange et al.76 evidenced that on a dehydrated surface that was exposed to moisture, 1 in 5 octadecylchlorosilane molecules is bonded to the surface. Due to this dense structure and full surface... [Pg.181]

Thermogravimetric analysis of nickel(II) chloride hexa-hydrate shows that water evolution occurs from ambient temperatures (25°) to 66.6°. The resulting dihydrate is stable up to 133.3°, beyond which temperature further water loss occurs. Differential thermal analysis shows an endotherm at 53.9° related to the first dehydration step, and a second, strong endotherm at 118.9°, not accompanied by any weight loss, indicates the transformation of an octahedrally coordinated to a close-packed cubic structure. [Pg.156]

Thermogravimetric analysis of a sample of the 5 hydrate shows that water evolution occurs between 34.1° and 89.6°, at which latter temperature a dihydrate has formed. This is stable up to 107°, beyond which temperature the remaining two water molecules are slowly lost. Differential thermal analysis shows two dehydration endotherms at 36.4 and 132.8° and a structure transformation (octahedrally coordinated to close-packed hexagonal) endotherm at 151.8°. [Pg.158]

In fine animal fibers, e.g., Merino wool, the structure develops solely from cuticle and cortical cells, but with increasing diameter a third type of cell becomes more prominent in the follicle. The medulla is formed from an axial stream of cells which do not become densely packed with protein or develop highly asymmetric shapes. By contrast the cell contents shrivel up during dehydration leaving a series of vacuoles along the fiber axis. [Pg.193]

Zeolites are microporous frameworks, and all of the ET chemistry that we have discussed is with molecules smaller than 13 A. The unique features of zeolites are their ion-exchanging ability, a stable structure upon dehydration and a pore/chan-nel structure that allows for a well-defined arrangement of molecules in space and the fact that redox-active atoms can be substituted on the framework. In most cases, the zeolite is an active host, influencing ET reactions via electrostatic fields or steric effects, a feature that is not found with the mesoporous and sol gel materials. Packing of molecules/ions in the intrazeolitic space with very high densities is also possible and was found to be important in charge propagation and electrochemistry. [Pg.2851]


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See also in sourсe #XX -- [ Pg.70 ]




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