Effect of water on the heat capacity of polymerized aluminosilicate glasses and melts

被引:37
作者
Bouhifd, MA
Whittington, A
Roux, J
Richet, P
机构
[1] Inst Phys Globe, UMR 7047, F-75252 Paris 05, France
[2] Univ Oxford, Dept Earth Sci, Oxford OX1 3PR, England
[3] Univ Missouri, Dept Geol Sci, Columbia, MO 65211 USA
关键词
D O I
10.1016/j.gca.2005.09.012
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The effect of water on heat capacity has been determined for four series of hydrated synthetic aluminosilicate glasses and supercooled liquids close to albite, phonolite, trachyte, and leucogranite compositions. Heat capacities were measured at atmospheric pressure by differential scanning calorimetry for water contents between 0 and 4.9 wt % from 300 K to about 100 K above the glass transition temperature (T-g). The partial molar heat capacity of water in polymerized aluminosilicate glasses, which can be considered as independent of composition, is (C-P) over bar (H2O) = -122.319 + 341.631 X 10(-3) T + 63.4426 x 10(5)/T-2 (J/mol K). In liquids containing at least 1 wt % H2O, the partial molar heat capacity of water is about 85 J/mol K. From speciation data, the effects of water as hydroxyl groups and as molecular water have tentatively been estimated, with partial molar heat capacities of 153 +/- 18 and 41 +/- 14 J/mol K, respectively. In all cases, water strongly increases the configurational heat capacity at T-g and exerts a marked depressing effect on T-g, in close agreement with the results of viscosity experiments on the same series of glasses. Consistent with the Adam and Gibbs theory of relaxation processes, the departure of the viscosity of hydrous melts from Arrhenian variations correlates with the magnitude of configurational heat capacities. (c) 2005 Elsevier Inc. All rights reserved.
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页码:711 / 722
页数:12
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