PARTIAL MOLAR VOLUME OF WATER IN PHONOLITIC GLASSES AND LIQUIDS

Show simple item record

dc.contributor.author Bouhifd A.
dc.contributor.author Whittington A.
dc.contributor.author Richet P.
dc.date.accessioned 2021-03-15T07:09:55Z
dc.date.available 2021-03-15T07:09:55Z
dc.date.issued 2001
dc.identifier https://www.elibrary.ru/item.asp?id=817672
dc.identifier.citation Contributions to Mineralogy and Petrology, 2001, 142, 2, 235-243
dc.identifier.issn 0010-7999
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/26728
dc.description.abstract The 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.title PARTIAL MOLAR VOLUME OF WATER IN PHONOLITIC GLASSES AND LIQUIDS
dc.type Статья


Files in this item

This item appears in the following Collection(s)

  • ELibrary
    Метаданные публикаций с сайта https://www.elibrary.ru

Show simple item record