THERMAL EXPANSION AND CRYSTAL STRUCTURE OF FeSi BETWEEN 4 AND 1173 K DETERMINED BY TIME-OF-FLIGHT NEUTRON POWDER DIFFRACTION

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dc.contributor.author Vočadlo L.
dc.contributor.author Price G.D.
dc.contributor.author Wood I.G.
dc.contributor.author Knight K.S.
dc.date.accessioned 2021-06-15T10:59:47Z
dc.date.available 2021-06-15T10:59:47Z
dc.date.issued 2002
dc.identifier https://elibrary.ru/item.asp?id=13908881
dc.identifier.citation Physics and Chemistry of Minerals, 2002, 29, 2, 132-139
dc.identifier.issn 0342-1791
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/29058
dc.description.abstract The thermal expansion and crystal structure of FeSi has been determined by neutron powder diffraction between 4 and 1173 K. No evidence was seen of any structural or magnetic transitions at low temperatures. The average volumetric thermal expansion coefficient above room temperature was found to be 4.85(5) × 10−5 K−1. The cell volume was fitted over the complete temperature range using Grüneisen approximations to the zero pressure equation of state, with the internal energy calculated via a Debye model; a Grüneisen second-order approximation gave the following parameters: θD=445(11) K, V 0=89.596(8) Å3, K 0′=4.4(4) and γ′=2.33(3), where θD is the Debye temperature, V 0 is V at T=0 K, K 0′ is the first derivative with respect to pressure of the incompressibility and γ′ is a Grüneisen parameter. The thermodynamic Grüneisen parameter, γth, has been calculated from experimental data in the range 4–400 K. The crystal structure was found to be almost invariant with temperature. The thermal vibrations of the Fe atoms are almost isotropic at all temperatures; those of the Si atoms become more anisotropic as the temperature increases.
dc.subject FeSi
dc.subject Thermal expantion
dc.subject Crystal structure
dc.subject Neutron diffraction
dc.title THERMAL EXPANSION AND CRYSTAL STRUCTURE OF FeSi BETWEEN 4 AND 1173 K DETERMINED BY TIME-OF-FLIGHT NEUTRON POWDER DIFFRACTION
dc.type Статья


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