SHOCK TEMPERATURES AND MELTING OF IRON AT EARTH CORE CONDITIONS

被引:281
作者
YOO, CS [1 ]
HOLMES, NC [1 ]
ROSS, M [1 ]
WEBB, DJ [1 ]
PIKE, C [1 ]
机构
[1] UNIV CALIF DAVIS,DEPT PHYS,DAVIS,CA 95616
关键词
D O I
10.1103/PhysRevLett.70.3931
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
The temperature of shock compressed iron has been measured to 340 GPa, using well characterized iron films sputtered on transparent diamond substrates and a 1 ns time-resolved optical method. We find a knee on the (P,T) iron Hugoniot indicating melting at 6350 K and 235 GPa and at 6720 K and 300 GPa. An extrapolation yields an iron melting temperature of 6830 (+/- 500) K at 330 GPa, the pressure of the Earth inner-outer core boundary. Implication of the melting data for the iron phase diagram is also discussed.
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页码:3931 / 3934
页数:4
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