SCALING OF THERMODYNAMIC MIXING PROPERTIES IN GARNET SOLID SOLUTIONS

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dc.contributor.author Bosenick A.
dc.contributor.author Dove M.T.
dc.contributor.author Heine V.
dc.contributor.author Geiger C.A.
dc.date.accessioned 2021-03-30T10:40:28Z
dc.date.available 2021-03-30T10:40:28Z
dc.date.issued 2001
dc.identifier https://www.elibrary.ru/item.asp?id=872456
dc.identifier.citation Physics and Chemistry of Minerals, 2001, 28, 3, 177-187
dc.identifier.issn 0342-1791
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/27175
dc.description.abstract The volumes and enthalpies of mixing, ΔV Mixd ΔHMixf binary solid-solution aluminosilicate garnets have been studied by computer simulation. The use of "average atoms" to simulate solid solution was found to give results that are considerably different from those obtained by calculating and averaging over many configurations of cations at a given composition. Although we expect mineral properties calculated from model calculations to be correct only on a qualitative rather than a quantitative scale, fair agreement with experiment was obtained where carefully tested potential parameters were used. The results show that mixing behaviour in these materials is controlled by local strain and relaxation effects resulting from the atomic size mismatch of the mixing divalent cations. In particular, ΔVMixd ΔHMixe shown to scale quadratically with the volume difference between the end members, and to vary essentially symmetrically with composition, with a moderate dependence on the degree and nature of cation order. We conclude that computer modelling should be useful in providing detailed qualitative information about the mixing properties of solid solutions, which can help to better constrain and interpret experimental results.
dc.subject ALUMINOSILICATE GARNETS
dc.subject COMPUTER SIMULATION
dc.subject SOLID SOLUTIONS
dc.subject MIXING PROPERTIES
dc.title SCALING OF THERMODYNAMIC MIXING PROPERTIES IN GARNET SOLID SOLUTIONS
dc.type Статья


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