RAMAN SPECTRA AND STRUCTURE OF BAO-SIO2, SRO-SIO2 AND CAO-SIO2 MELTS TO 1600°C

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dc.contributor.author Frantz J.D.
dc.contributor.author Mysen B.O.
dc.date.accessioned 2020-11-24T04:34:52Z
dc.date.available 2020-11-24T04:34:52Z
dc.date.issued 1995
dc.identifier https://elibrary.ru/item.asp?id=656418
dc.identifier.citation Chemical Geology, 1995, , 1, 155-176
dc.identifier.issn 0009-2541
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/19473
dc.description.abstract Raman spectra were collected for barium silicate, strontium silicate and calcium silicate melts at temperatures ranging from the glass transition region to temperatures as high as 1600°C. For melts less polymrized than disilicate, the spectra were used to determine the relative abundances of the Q3, Q2 and Q1 tetrahedra and the Si2O2-5, SiO2-3 and Si2O6-77 structural units in the melts. A concentration constant was computed for the reaction: 4SiO2-3 # Si2O2-5 + Si2O6-7 and was found to vary with composition from approximately log10 Kc = 0.5 for barium silicate melts with NBO/Si = 1.143 to log10 Kc = -1.75 for calcium metasilicate melts with NBO/Si = 2. Little difference was found to exist in the structural behavior of the melts on the three alkaline-earth silicate binary joins. Activity coefficients were computed for the SiO2-3 structural unit as a function of bulk composition. The logarithm of the activity coefficients and mole fraction of the structural unit are linearly correlated.
dc.title RAMAN SPECTRA AND STRUCTURE OF BAO-SIO2, SRO-SIO2 AND CAO-SIO2 MELTS TO 1600°C
dc.type Статья


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