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Silicate glasses heat capacity

Stebbins I F, Carmichael I. S. E. and Moret L. K. (1984). Heat capacities and entropies of silicate liquids and glasses. Contrib. Mineral Petrol, 86 132-148. [Pg.855]

Owing to their polymeric nature, many silicate compounds and systems tend to form glasses. When cooling rapidly from the molten state, a part of the sample crystallizes, while the other part remains glassy. This is the main disadvantage while measuring their heat capacity, heat content, enthalpy of fusion, and mixing. [Pg.251]

The mean isobaric specific heat capacities Cp (2Q°C 100 °C) listed in Table 3.4-16c were measured from the heat transfer from a hot glass sample at 100 °C into a liquid calorimeter at 20°C. The values of Cp 20°C 100 °C) and also of the true thermal capacity Cp 20 °C) for silicate glasses range from 0.42 to 0.84 J/gK. [Pg.556]


See other pages where Silicate glasses heat capacity is mentioned: [Pg.267]    [Pg.433]    [Pg.7]    [Pg.102]    [Pg.125]    [Pg.156]    [Pg.125]    [Pg.451]    [Pg.372]    [Pg.117]    [Pg.141]    [Pg.337]    [Pg.169]    [Pg.146]   
See also in sourсe #XX -- [ Pg.263 ]




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