1. Shock temperatures and melting of iron at Earth core conditions
- Author
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D. J. Webb, N. C. Holmes, C. R. Pike, Choong-Shik Yoo, and Marvin Ross
- Subjects
Core (optical fiber) ,Shock wave ,Materials science ,Transition metal ,Transition temperature ,engineering ,General Physics and Astronomy ,Diamond ,Thermodynamics ,engineering.material ,Earth (classical element) ,Phase diagram ,Shock (mechanics) - Abstract
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 (\ifmmode\pm\else\textpm\fi{} 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.
- Published
- 1993
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