Pure Iron Compressed and Heated to Extreme Conditions
ORAL
Abstract
The results of a first-principles study supported by the temperature-quenched laser-heated diamond anvil-cell experiments on the high-pressure high-temperature structural behavior of pure iron are reported. We show that in contrast to the widely accepted picture, the face-centered cubic (fcc) phase becomes as stable as the hexagonal-close-packed (hcp) phase at pressures around 300–360 GPa and temperatures around 5000–6000 K. Our temperature-quenched experiments indicate that the fcc phase of iron can exist in the pressure-temperature region above 160 GPa and 3700 K, respectively. This, in particular, means that the actual structure of the Earth's core may be a complex phase with a large number of stacking faults.
*Acknowledgement to the ESF program ``Mineralogy and Chemistry of Earth's core (MCEC)", Swedish Research Council (VR), Swedish Foundation for Strategic Research (SSF), Swedish National Infrastructure for Computing (SNIC), Deutsche Forschungsgemeinschaf
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Authors
Arkady Mikhaylushkin
Theory and Modeling Division, Department of Physics, Chemistry and Biology (IFM), Link\"oping University, S-581 83, Link\"oping, Sweden
Department of Physics, Chemistry and Biology, Linkoping University, Sweden
Sergei Simak
Department of Physics, Chemistry and Biology, Linkoping University, Sweden
Theory and Modeling Division, Department of Physics, Chemistry and Biology (IFM), Link\"oping University, S-581 83, Link\"oping, Sweden