Page 459 - Carrahers_Polymer_Chemistry,_Eighth_Edition
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     422                                                    Carraher’s Polymer Chemistry
                 solid is forced outward as collapse occurs. The frictional forces caused by the gas passing through
                 a restricted opening are indirectly proportional to the square of the pore diameter. Because the pore
                 sizes are so small, the rapidly moving gas also absorbs a lot of the energy. Thus, energy is absorbed
                 by the aerogel through both collapse of the solid network structure and release of the gas within the
                 aerogel.
                    Aerogels that are about 2–5 nm in diameter have large surface to volume ratios on the order of
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                   9
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                 10  meters  and high specific surface areas approaching 1,000 m /g. Such large surface to volume
                 ratios makes the surface particularly active and potential materials as catalysts, absorbents, and
                 catalyst substrates.
                    The precise chemical makeup of the surface depends on the materials used to make the aerogel
                 and the method of processing. Typical aerogel sequences produce products whose surfaces are rich in
                 hydroxyl groups. Because of the high surface area, -Si-OH groups act as weak acids and are reactive
                 in typical Lewis acid–base reactions. As noted before, aerogels have many hydrogen-bonding hydrox-
                 yls at their surface making aerogels extremely hygroscopic. Dry aerogel materials will increase their
                 weight by 20% through uptake of moisture from the air. This absorption is reversible and appears to
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                 have little or no effect on the aerogel. Water is removed through heating to 100 C–120 C.
                    While adsorption of water vapor has little effect on aerogels, contact with liquid water has dev-
                 astating effects on aerogels. When water enters the nanometer-size pores, the surface tension of the
                 water exerts capillary forces sufficient to fracture the silica backbone, resulting is a collapse of the
                 complex matrix structure. This tendency to be attacked by water is overcome through conversion of
                 the surface polar –OH groups to nonpolar –OR groups. The “R” is typically a trimethylsilyl group
                 though any aliphatic group would work. Conversion can be accomplished within the wet stage
                 (preaerogel) or after the supercritical drying. These treatments result in an aerogel that is called
                 “hydrophobic” aerogel, which is stable in water.
                    The pore size of aerogels varies. The International Union of Pure and Applied Chemistry clas-
                 sifies materials with pore sizes of less that 2 nm as “micropores,” 2–50 nm are called “mesopores,”
                 and those greater than 50 nm in diameter are called “macropores.” While aerogels have some pores
                 that fall within the micropore region, the majority of pores are in the mesopore region.
                    Most of the aerogels produced today are described as being transparent. While it might be
                 assumed that since aerogels are made of the same material as window glass and quartz (SiO ) that
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                 they would be transparent, this is not necessarily the case. Transparency requires a number of fac-
                 tors. Thus, so-called smokey and white quarts are colored because of the presence of impurities.
                 Mixtures of amorphous and crystalline silicon dioxide can be made that are not transparent. The
                 size and distribution of reflecting and refractive sites are important factors in determining if a mate-
                 rial is transparent with the theme of “sameness” contributing to making a material transparent.
                    The majority of light we see is scattered light, that is, light that reaches our eyes in an indi-
                 rect manner. The scattering phenomenon is what gives us blue skies, white to gray clouds, and
                 poor visibility in fog. This scattering is not simply reflecting but results from the interaction of
                 light with an inhomogeneous site. Light-scattering photometry is used to determine the size of
                 polymers. Scattering is most effective when the scattering particle size is about that of the wave
                 length of the light. For visible light, this occurs with scattering sites that are about 400–700 nm.
                 Scattering centers that are much less in size than the incoming light wavelength are much less
                 effective at scattering the light. Since the particle sizes in an aerogel are much smaller than the
                 individual sites they are ineffective scattering sites. Similar to classical polymer chains, where
                 the entire chain or segments of the entire chain act as a scattering site, clusters of individual sites
                 within the aerogel act as scattering sites. Most of these scattering sites are again smaller than
                 the wavelength of visible light, but some are within the range to scatter visible light so that a
                 soft reflected light results. The different-sized scattering sites and variable wavelengths present
                 in visible light cause a reddening of the transmitted light (red light has a longer wavelength and
                 is scattered less by small clusters present in the aerogel), resulting in the blue appearance of the
                 reflected light from the aerogel.
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