Gruneisen parameter of ε-iron up to 300 GPa from in-situ X-ray study

被引:43
作者
Dubrovinsky, LS [1 ]
Saxena, SK
Dubrovinskaia, NA
Rekhi, S
le Bihan, T
机构
[1] Uppsala Univ, Inst Earth Sci, S-75236 Uppsala, Sweden
[2] European Synchrotron Radiat Facil, F-38043 Grenoble, France
关键词
D O I
10.2138/am-2000-2-318
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We show that high-quality powder X-ray diffraction data, collected in diamond anvil cells, provide sufficient information for Rietveld refinement and determination of temperature factors. For the first time using a new method based on combination of thermal equation of state and measured mean-square atomic vibrations of high-pressure epsilon-Fe phase, we determine Debye temperatures at pressure up to 300 GPa and temperature over 1000 K. We found that the Gruneisen parameter of epsilon-iron could be described by Anderson's (1967) equation with parameters gamma(0) = 1.78(6), q = 0.69(10) with fixed V-0 = 6.73 cm(3)/mol.
引用
收藏
页码:386 / 389
页数:4
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