Zobrazeno 1 - 10
of 124
pro vyhledávání: '"Y. Bottinga"'
Autor:
Donald G. Fraser, Y. Bottinga
The apparent differences between heats of mixing determined by solution calorimetric measurements on quenched samples in the system NaAlSi 3 O 8 -KAlSi 3 O 8 and heats of mixing determined at high temperatures by Knudsen cell mass spectrometry are ca
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1968310bef3b8c56ff5c8e67077568b6
https://doi.org/10.1016/0016-7037(85)90288-1
https://doi.org/10.1016/0016-7037(85)90288-1
Publikováno v:
Journal of Non-Crystalline Solids. 290:129-144
Time-dependent variations of the viscosity of silicate melts, associated with sudden changes of temperature or uniaxial compressive stress, have been measured. The melt compositions were MgCaSi2O6, CaAl2Si2O8 and NaAlSi3O8. The steady-state viscosity
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0505a965938c77d898711d68b6ef44c1
https://doi.org/10.1016/s0022-3093(01)00709-8
https://doi.org/10.1016/s0022-3093(01)00709-8
Publikováno v:
Journal of Non-Crystalline Solids. 288:166-174
The Adam–Gibbs and the Vogel–Tamman–Fulcher equations are very often used to express the temperature dependence of the viscosity of liquids. Both equations reproduce very well the same sets of viscosity measurements, but the adjustable constant
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5dceedc0e08eab383663b55277548490
https://doi.org/10.1016/s0022-3093(01)00527-0
https://doi.org/10.1016/s0022-3093(01)00527-0
Publikováno v:
Earth and Planetary Science Letters. 160:537-550
The study of glass inclusions inside mantle minerals provides direct information about the chemistry of naturally occurring mantle-derived melts and the fine-scale complexity of the melting process responsible for their genesis. Minerals in a spinel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cfd29f32da1ac360a3f66e84da86b30e
https://doi.org/10.1016/s0012-821x(98)00109-5
https://doi.org/10.1016/s0012-821x(98)00109-5
Akademický článek
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Publikováno v:
Chemical Geology. 128:1-4
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::477192743ec95000ef752b78f935188d
https://doi.org/10.1016/0009-2541(95)00158-1
https://doi.org/10.1016/0009-2541(95)00158-1
Autor:
Pascal Richet, Y. Bottinga
Publikováno v:
Chemical Geology. 128:129-141
Several applications of the Adam-Gibbs theory of relaxation processes in viscous liquids to the theology of silicate melts are reviewed. This theory reproduces very well the isostructural viscosity observations, it explains the occurrence of shear th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5ab02e3d04f605eb5ba1b6c31a088f79
https://doi.org/10.1016/0009-2541(95)00168-9
https://doi.org/10.1016/0009-2541(95)00168-9
Autor:
Y. Bottinga, Pascal Richet
Publikováno v:
Geochimica et Cosmochimica Acta. 59:2725-2731
The decrease of the specific volume, when the extent of polymerization diminishes, is a cause of the pressure sensitivity of the viscosity of silicate melts. This effect can be explained by means of the Adam and Gibbs (1965) theory, taking into accou
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2e2d378d62f29b6c1c194475e7f690ac
https://doi.org/10.1016/0016-7037(95)00168-y
https://doi.org/10.1016/0016-7037(95)00168-y
Autor:
Y. Bottinga
Publikováno v:
Journal of Geophysical Research: Solid Earth. 99:9415-9422
Homogeneous silicate liquids have a Newtonian rheology under conditions of modest stress, but under relatively high stress or otherwise imposed high rates of deformation their viscosity may become non-Newtonian before the onset of rupture. This behav
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eefedc3689654489335f2b7131aea2a4
https://doi.org/10.1029/94jb00135
https://doi.org/10.1029/94jb00135
Publikováno v:
Chemical Geology. 174:1-3
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4dbb8370546238ae0d3e68070ca13646
https://doi.org/10.1016/s0009-2541(00)00302-8
https://doi.org/10.1016/s0009-2541(00)00302-8