Radiographic study on the viscosity of the Fe-FeS melts at the pressure of 5 to 7 GPa

被引:0
|
作者
Urakawa, S
Terasaki, H
Funakoshi, K
Kato, T
Suzuki, A
机构
[1] Okayama Univ, Dept Earth Sci, Okayama 7008530, Japan
[2] Univ Tsukuba, Inst Geosci, Tsukuba, Ibaraki 3058571, Japan
[3] Japan Synchrotron Radiat Res Inst, Mihara 6795198, Japan
[4] Tohoku Univ, Inst Mineral Petrol & Econ Geol, Sendai, Miyagi 9808578, Japan
关键词
D O I
10.2138/am-2001-0420
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
Stokes' viscometry combined with in situ X-ray radiographic observation, using the 6-8 type multi-anvil press and synchrotron radiation, has been applied to the viscosity measurement of the Fe-FeS melt up to pressures of 7 GPa. The viscosity is found to be about 2 x 10(-2) Pa-s at 5 to 7 GPa and temperatures about 1350 K, in marked contrast to previous viscosity measurements, which showed high viscosity, 0.5 to 14 Pa-s, at 2 to 5 GPa (LeBlanc and Secco 1996). Our viscosity data, however, is consistent with all other evidence, which include 1 atm viscosity data, X-ray structure analysis, and ab initio simulations. Recent viscosity measurements (Dobson et al. 2000) also showed the viscosity of Fe-FeS melt to be about 10(-2) Pa-s at 2.5 GPa. Thus, we are confident that the viscosity of the Fe-FeS melt is close to a typical value (10(-2) Pa-s) of viscosity for liquid metal even at high pressures.
引用
收藏
页码:578 / 582
页数:5
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