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American Mineralogist; November-December 2009; v. 94; no. 11-12; p. 1591-1595; DOI: 10.2138/am.2009.3240
© 2009 Mineralogical Society of America
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Influence of cation size on the low-temperature heat capacity of alkaline earth metasilicate glasses

Pascal Richet1,*, Atsusi Nidaira1, Daniel R. Neuville2 and Tooru Atake1

1 Materials and Structures Laboratory, Tokyo Institute of Technology, 4259 Nagatsuta-cho, Midori-ku, Yokohama, 226-8503 Japan
2 Physique des Minéraux et des Magmas, Institut de Physique du Globe, 4 place Jussieu, 75252 Paris cedex 05, France

Correspondence: * Permanent address: Physique des Minéraux et des Magmas, Institut de Physique du Globe, 4 place Jussieu, 75252 Paris cedex 05, France. E-mail: richet{at}ipgp.jussieu.fr

The heat capacities of Sr and Ba metasilicate glasses and of a Mg silicate glass with only 44 mol% SiO2 have been measured between 2 and 300 K with the Quantum Design Physical Property Measurement System. The derived vibrational entropies S298-S0 are 50.90, 61.00, and 36.65 J/(mol · K) for Sr0.5Si0.5O1.5, Ba0.5Si0.5O1.5, and Mg0.56Si0.44O1.44 glasses, respectively. Along with available data for Mg- and Ca-bearing glasses, these results indicate a regular variation of the partial molar vibrational entropy of the metal oxide as a function of the ionization potential of the cation. At very low temperatures, however, the excess heat capacity of barium metasilicate glass relative to Debye limiting T3 law is stronger than expected from such a trend, whereas Mg1.12Si0.88O2.88 is the known glass whose CP deviates the less from this law.

Key Words: Heat capacity • entropy • alkaline earth silicate glasses







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