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  • 1935-1939  (2)
  • Chemistry/Pharmacy  (2)
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  • 1935-1939  (2)
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  • Chemistry/Pharmacy  (2)
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  • 1
    Online Resource
    Online Resource
    Wiley ; 1935
    In:  Journal of the American Ceramic Society Vol. 18, No. 1-12 ( 1935-12), p. 289-296
    In: Journal of the American Ceramic Society, Wiley, Vol. 18, No. 1-12 ( 1935-12), p. 289-296
    Abstract: The progress of fusion in an alluvial clay, a glacial clay, and a shale, when heated at various temperatures, was determined with the aid of the petrographic microscope. Thin sections and powdered samples obtained from the heated clay specimens were used in these tests. The relationships between the amounts and kinds of glasses in the specimens and the properties of the glasses were determined. Shrinkage and porosity of the specimens were found to depend not only on the temperature at which glass formation started but also on that at which the glass became sufficiently fluid to allow contraction of the specimen to take place. The colors of the heated clay specimens were governed largely by the crystallization of the glass bonds. Solution of the crystals formed by devitrification also profoundly affected the colors of the specimens. The increase in intensity of the red color of the specimens of alluvial clay and shale was directly related to the increase in the number of red crystals produced in the glass phases. The loss of red color by these specimens heated at very high temperatures in an oxidizing atmosphere and also at lower temperatures in a reducing atmosphere was caused by solution of the red crystals. The glassy bond in the specimens of glacial clay differed in composition from that in the alluvial clay and shale, which prevented the development of a red color of the specimens. A black glass, formed on solution of the red crystals, produced a dark gray color in the overheated specimens and in those heated in a reducing atmosphere. The growth of fine‐grained green crystals in the glacial clay specimens was a factor in neutralizing the small amount of red color originally in these test pieces.
    Type of Medium: Online Resource
    ISSN: 0002-7820 , 1551-2916
    URL: Issue
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1935
    detail.hit.zdb_id: 2008170-4
    detail.hit.zdb_id: 219232-9
    Location Call Number Limitation Availability
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  • 2
    Online Resource
    Online Resource
    Wiley ; 1939
    In:  Journal of the American Ceramic Society Vol. 22, No. 1-12 ( 1939-12), p. 1-8
    In: Journal of the American Ceramic Society, Wiley, Vol. 22, No. 1-12 ( 1939-12), p. 1-8
    Abstract: The mechanisms of viscous flow and of electrolytic conduction in liquids have been examined to show the significance of the activation energy which is evaluated from the temperature coefficients of viscosity and electrical resistivity. It is shown that the high numerical values characteristic of silicate glasses arise from the ionic character of the liquid, the small coordination number (4) for silicon, and the high electric charge on the ions (Si, 4; 0,2; etc.). Below the softening range, a glass is not necessarily stabilized ( i.e. , in equilibrium with respect to molecular association or dissociation processes) and its properties depend on its history, mechanical, thermal, etc. In stabilized glasses, the activation energies for viscosity and electric resistivity rise continually with falling temperatures, showing no maximum, in contrast to the views of Preston and Seddon. The oxygen, to silicon ratio has a dominating rôle in the structure of silicate crystals, as shown by W. L. Bragg. Similar concepts are applied to glass, and it is shown that the Preston‐Seddon proposal of definite compounds in soda‐silica glasses may be replaced by an alternate explanation. The quantity, β, in the equation, η= ar β, which relates viscosity to resistivity, has a value of 4 to 6 for certain soda‐containing glasses. The suggestion is made that viscous shear requires the breaking of four to six times as many sodium‐oxygen bonds as does electrical conduction. Finally, an internal energy‐temperature curve, based on specific‐heat data for fused silica, has been constructed. The curve shows a. steady rise with increasing temperature. It is typical of several glasses.
    Type of Medium: Online Resource
    ISSN: 0002-7820 , 1551-2916
    URL: Issue
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1939
    detail.hit.zdb_id: 2008170-4
    detail.hit.zdb_id: 219232-9
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
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