Mineralogical Journal
Online ISSN : 1881-4174
Print ISSN : 0544-2540
ISSN-L : 0544-2540
 
Structures of hydrated glasses in the albite-anorthite-quartz system
M. OKUNOF. MARUMOH. MORIKAWAS. NAKASHIMAJ. T. IIYAMA
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ジャーナル フリー

1987 年 13 巻 7 号 p. 434-442

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Aluminosilicate glasses containing H2O (NaAlSi3O8·1.88H2O, Na0.57Al0.57Si3.43O8·1.69H2O, Ca0.38Al0.77Si3.23O8·1.71H2O) were synthesized by the hydrothermal method, and their structures were studied by the X-ray diffraction method. All of these glasses have TO4 (T = Si, Al) tetrahedra as basic structure units like in anhydrous aluminosilicate glasses. However, shapes of correlation functions are different from those of the corresponding anhydrous ones in the longer range than 3.5Å. Main structural changes induced by the addition of H2O are breakdown of linkage of TO4 tetrahedra to form clusters.
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© 1987 Japan Association of Mineralogical Sciences
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