Encyclopedia of Glass Science, Technology, History, and Culture. Группа авторов

Encyclopedia of Glass Science, Technology, History, and Culture - Группа авторов


Скачать книгу
the liquid must undergo a phase transition before reaching it. This is, of course, the glass transition. In its original form, Kauzmann's paradox implicitly neglects possible differences in vibrational entropy between the amorphous and crystalline phases. This simplification is actually incorrect but it does not detract from the gist of the argument, for taking into account such differences would only shift TK slightly. A more rigorous statement of the paradox is that the catastrophe would occur when the configurational entropy of the supercooled liquid vanishes.

      2.4.6 Potential Energy Landscape: Ideal Glass and Fragility

      Among the great many statistical mechanical models that have attempted to account for the glass transition and solve Kauzmann's paradox, the early one proposed by Gibbs and Di Marzio [48] is of special interest. It predicts that the supercooled liquid would transform to an ideal glass through a second‐order transition at the temperature T0 at which its configurational entropy would vanish. Since then, the existence and the nature of such a transformation have been much debated. This debate notwithstanding, the important point for our discussion is the result subsequently derived by Adam and Gibbs [49] on the basis of a lattice model of polymers. This result is a very simple relationship between relaxation times and the configurational entropy of the melt, viz.

      (10)equation

      where Ae is a pre‐exponential term and Be is approximately a constant proportional to the Gibbs free energy barriers hindering the cooperative rearrangements of the structure.

      Qualitatively, this theory assumes that structural rearrangements would be impossible in a liquid with zero configurational entropy so that relaxation time would be infinite. If two configurations only were available for an entire liquid volume, mass transfer would require a simultaneous displacement of all structural entities. The probability for such a cooperative event would be extremely small, but not zero, and the relaxation times would be extremely high, but no longer infinite. When configurational entropy increases, the cooperative rearrangements of the structure required for mass transfer can take place independently in smaller and smaller regions of the liquid.

Graphs depict the fragility as a measure of the extent of temperature-induced configurational changes in inorganic and organic glass-forming liquids: correlations between relative Cp increases at the glass transition and deviations of viscosities from Arrhenius laws. Lower panel, from top to bottom: SiO2, GeO2, BeF3, ZnCl3, LiCH3COO, 4 Ca[(NO3)]2·4 H2O, o-terphenyl, glycerol (C3H8O3), and H2SO4·3 H2O.

      (Source: After [52]).

      Lower panel, from top to bottom: SiO2, GeO2, BeF3, ZnCl3, LiCH3COO, 4 Ca[(NO3)]2·4 H2O, o‐terphenyl, glycerol (C3H8O3), and H2SO4·3 H2O.

      1 Bontemps, G. (1868). Guide du verrier. Traité historique et pratique de la fabrication des verres, cristaux, vitraux, 1. Paris: Librairie du dictionnaire des arts et manufactures (trans. Cable, M. (2008). Bontemps on Glass Making. Sheffield: Society of Glass Technology).

      2 Figuier, L. (1873). Les Merveilles de l'industrie ou description des principales industries modernes [The Wonders of Industry or Description of the Main Modern Industries], vol. 1, 156–157. Paris: Furne, Jouvet et Cie.

      3 Richet, P. (2000). L'Âge du verre [The Glass Age]. Paris: Gallimard.

      4 Morse, D.L. and Evenson, J.W. (2016). Welcome to the glass age. Int. J. Appl. Glass Sci. 7: 409–412.

      5 Cann, J.R. and Renfrew, C. (1964). The characterization of obsidian and its application to the Mediterranean region. Proc. Prehist. Soc. 30: 111–133.

      6 Gasparyan, B. and Arimura, M. (eds.) (2014). Stone Age of Armenia. A Guide‐Book to the Stone Age Archaeology in the Republic of Armenia. Kamazawa: Kamazawa University.

      7 Shea, J.J. (2013). Stone Tools in the Paleolithic and Neolithic near East: A Guide. Cambridge: Cambridge University Press.

      8 Adler, D.S., Wilkinson, K.N., Bloc, S. et al. (2014). Early Levallois technology and the lower to middle Paleolithic transition in the southern Caucasus. Science 345: 1609–1613.

      9 Glauberman, P., Gasparian, B., Wilkinson, K. et al. (2016). Introducing Barozh 12: a middle Palaeolithic open‐air site on the edge of the Ararat depression, Armenia. ARAMAZD, Armenian J. Near‐East. Stud. 9 (2016): 7–20.

      10 Petronius Arbiter, 51 (repr. 1987). Satyricon (trans. M. Heseltine). Cambridge: Harvard University Press.

      11 Shortland, A., Schachner, L., Freestone, I., and Tite, M. (2006). Natron as a flux in the early vitreous materials industry: sources, beginings and reasons for decline. J. Archaeol. Sci. 33: 521–530.

      12 Stern, E.M. (1999). Roman glass blowing in a cultural context. Am. J. Archaeol. 103: 441–484.

      13 Lomonosov, M.V. (1967). Pis'mo o pol'ze stekla (trans. H.B. Segel, Letter on the Use of Glass, 209–220 in The Literature of Eighteenth‐Century Russia). New York: E.P. Dutton & Co.

      14 Figuier, L. (1868). Les Merveilles de la science ou Description populaire des inventions modernes [The Wonders of Science or Popular Description of Modern Inventions], vol. I, 463. Paris: Furne, Jouvet et Cie.

      15 Franklin, B. (1769). Letter to Giambatista Beccaria. In: Experiments and Observations on Electricity, Made at Philadelphia in America, to Which Are Added Letters and Papers on Philosophical Subjects, 4e, 427–433. London: D. Henry.

      16 Mozart, W.A. Adagio in C for armonica (K. 356); Adagio and Rondo in C minor for armonica, flute, oboe, viola and cello (K. 617).

      17 Cohen, A. (1981). Music in the French Royal Academy of Sciences: A Study in the Evolution of Musical Thought. Princeton University Press: Princeton.

      18 Powell, A. (2002). The Flute. Yale: Yale University Press.

      19 Knauth,


Скачать книгу