期刊
PHYSICS AND CHEMISTRY OF MINERALS
卷 29, 期 2, 页码 132-139出版社
SPRINGER
DOI: 10.1007/s002690100202
关键词
FeSi; thermal expansion; crystal structure; neutron diffraction
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(15) x 10(-5) K(-1). The cell volume was fitted over the complete temperature range using Gruneisen approximations to the zero pressure equation of state, with the internal energy calculated via a Debye model; a Gruneisen second-order approximation gave the following parameters : theta(D) = 445(11) K, V(0) = 89.596(8) Angstrom(3), K'(0) = (41) le tempe and gamma = 2.33(3), where theta(D) 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 gamma is a Gruneisen parameter. The thermodynamic Gruneisen parameter, 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.
作者
我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。
推荐
暂无数据