PARTIAL MOLAR VOLUME OF WATER IN PHONOLITIC GLASSES AND LIQUIDS

dc.contributor.authorBouhifd A.
dc.contributor.authorWhittington A.
dc.contributor.authorRichet P.
dc.date.accessioned2021-03-15T07:09:55Z
dc.date.available2021-03-15T07:09:55Z
dc.date.issued2001
dc.description.abstractThe volumes and expansivities of four hydrous phonolite glasses and liquids have been measured by dilatometry from 300 K up to the glass transition and over a 50 K interval just above the glass transition. The partial molar volume of water is independent of the water content for the glass and liquid phases, with values of about 11.0±0.5 and 17.1±0.9 cm3l at 300 and 800 K, respectively. The partial molar thermal expansivity of water in phonolite glasses is about 8×10-5 K^-1, a result similar to recently published values for different silicate compositions, and about 36.5×10-5 K-1 in phonolite liquids. The implications for melt density and water dissolution are discussed.
dc.identifierhttps://www.elibrary.ru/item.asp?id=817672
dc.identifier.citationContributions to Mineralogy and Petrology, 2001, 142, 2, 235-243
dc.identifier.issn0010-7999
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/26728
dc.titlePARTIAL MOLAR VOLUME OF WATER IN PHONOLITIC GLASSES AND LIQUIDS
dc.typeСтатья

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