X-ray evidence for the new phase β-iron at high temperature and high pressure

Details X-ray evidence for the new phase β-iron at high temperature and high pressure X-ray evidence for the new phase β-iron at high temperature and high pressure

Sep 1996

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1996georl..23.2441s&link_type=abstract

Geophysical Research Letters, Volume 23, Issue 18, p. 2441-2444

Physics

23

Geodesy And Gravity: Earth'S Interior-Composition And State, Mineral Physics, Mineral Physics: High-Pressure Behavior, Mineral Physics: X Ray, Neutron, And Electron Spectroscopy And Diffraction

Scientific paper

X-ray synchrotron study of iron heated between 1400 to 2200 K over a pressure range of 40 to 60 gigapascals confirms previous reports of the transformation of the hexagonal closest packed (HCP) phase of iron (ɛ) to the double HCP Iron (β). The study extends the stability range of the new phase β to the highest pressure range yet achieved for such transformation.

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