4.3 Article

Compression of Fe88.1Ni9.1S2.8 alloy up to the pressure of Earth's inner core

Journal

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2011JB008745

Keywords

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Funding

  1. Ministry of Education, Culture, Sports, Science, and Technology of the Japanese Government [21740374, 23684038, 22000002]
  2. Global Education and Research Center for Earth and Planetary Dynamics
  3. [2008A1601]
  4. [2008B1582]
  5. [2008B1625]
  6. [2009A1463]
  7. [2009A1570]
  8. [2009B0028]
  9. Grants-in-Aid for Scientific Research [23654181, 23340159, 21740374, 23684038, 20103003, 22000002, 22340164] Funding Source: KAKEN

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Fe88.1Ni9.1S2.8 alloy was compressed up to 335 GPa, corresponding to the pressure at the Earth's inner core, and the hexagonal close-packed structure was found to be stable. The axial (c/a) ratio gradually decreased with increasing pressure. A linear fit as a function of pressure gave c/a = 1.605(2)-6.1(9) x 10(-5)P for P in GPa. The compression curve of Fe88.1Ni9.1S2.8 alloy was expressed by the third-order Birch-Murnaghan equation of state, giving K-0 = 167.0 +/- 15.0 GPa, K-0' = 4.46 +/- 0.14, and V-0 = 22.93 +/- 0.29 angstrom(3). Our results indicate that the hcp Fe-5 wt % Ni-5.7 wt % S alloy can account for the density of the inner core at 328.9 GPa, assuming a linear relationship exists between the density and the nickel and sulfur content.

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