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Alpha-tridymite

CAS/DOT IDENTIFICATION 15468-32-3/none SYNONYMS alpha-tridymite, christensenite, tridymite, tridymite 118. [Pg.887]

At a temperature of 870°C, a-quartz transforms irreversibly into alpha-tridymite (a-tri-dymite, orthorhombic) [15468-32-3] with an important volume change of 14.4 vol.% as follows ... [Pg.594]

However, if the temperature is raised to 1470°C, a-tridymite transforms also irreversibly into alpha-cristoballite (a-cristoballite) without any change in volume as follows ... [Pg.594]

While tridymite and cristobalite may exist for indefinite periods of time at room temperature, tire low-temperature alpha-quartz is believed to be the form of silica truly stable at these temperatures. A considerable expansion accompanies the conversion of a-cristobalite to /J-cristobalite at 220-275°C, and a sudden expansion of -2.2% occurs during the inversion of a-quartz at 573°C. The conversion of quartz to tridymite at 870°C is accompanied by an expansion of -15%. [Pg.779]


See other pages where Alpha-tridymite is mentioned: [Pg.174]    [Pg.174]    [Pg.196]    [Pg.2406]    [Pg.506]    [Pg.13]    [Pg.93]    [Pg.95]   
See also in sourсe #XX -- [ Pg.594 ]




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Tridymite

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