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Title: Phase relations of Fe3C and Fe7C3 up to 185 GPa and 5200 K: Implication for the stability of iron carbide in the Earth's core

Abstract

We have investigated phase relations and melting behavior of Fe3C and Fe7C3 using X-ray diffraction in a laser-heated diamond cell up to 185 GPa and 5200 K. Our results show that the starting Fe3C sample decomposes into a mixture of solid orthorhombic Fe7C3 and hcp-Fe at above 145 GPa upon laser heating and then transforms into Fe-C liquid and solid Fe7C3 at temperatures above 3400 K. Using the intensity of the diffuse scattering as a primary criteria for detecting melting, the experimentally derived liquidus for a bulk composition of Fe3C fitted with the Simon-Glatzel equation is Tm(K) = 1800 × [1 + (Pm-5.7)/15.10 ± 2.55]1/2.41 ± 0.17 at 24–185 GPa, which is ~500 K higher than the melting curve of iron reported by Anzellini et al. (2013) at Earth's core pressures. The higher melting point and relative stability of Fe7C3 in Fe-rich Fe-C system at Earth's core conditions indicate that Fe7C3 could solidify out of the early Earth's molten core to become a constituent of the innermost inner core.

Authors:
ORCiD logo [1]; ORCiD logo [2]; ORCiD logo [3]; ORCiD logo [3]; ORCiD logo [4]
  1. Univ. of Texas, Austin, TX (United States). Jackson School of Geosciences, Dept. of Geological Sciences; Stanford Univ., CA (United States). Dept. of Geological Sciences
  2. Univ. of Texas, Austin, TX (United States). Jackson School of Geosciences, Dept. of Geological Sciences; Center for High Pressure Science and Technology Advanced Research, Shanghai (China)
  3. Univ. of Chicago, IL (United States). Consortium for Advanced Radiation Sources
  4. Okayama Univ., Okayama (Japan). Inst. for Planetary Materials
Publication Date:
Research Org.:
Univ. of Chicago, IL (United States)
Sponsoring Org.:
USDOE
OSTI Identifier:
1465341
Grant/Contract Number:  
FG02-94ER14466
Resource Type:
Accepted Manuscript
Journal Name:
Geophysical Research Letters
Additional Journal Information:
Journal Volume: 43; Journal Issue: 24; Journal ID: ISSN 0094-8276
Publisher:
American Geophysical Union
Country of Publication:
United States
Language:
English
Subject:
58 GEOSCIENCES

Citation Formats

Liu, Jin, Lin, Jung-Fu, Prakapenka, Vitali B., Prescher, Clemens, and Yoshino, Takashi. Phase relations of Fe3C and Fe7C3 up to 185 GPa and 5200 K: Implication for the stability of iron carbide in the Earth's core. United States: N. p., 2016. Web. doi:10.1002/2016GL071353.
Liu, Jin, Lin, Jung-Fu, Prakapenka, Vitali B., Prescher, Clemens, & Yoshino, Takashi. Phase relations of Fe3C and Fe7C3 up to 185 GPa and 5200 K: Implication for the stability of iron carbide in the Earth's core. United States. https://doi.org/10.1002/2016GL071353
Liu, Jin, Lin, Jung-Fu, Prakapenka, Vitali B., Prescher, Clemens, and Yoshino, Takashi. Wed . "Phase relations of Fe3C and Fe7C3 up to 185 GPa and 5200 K: Implication for the stability of iron carbide in the Earth's core". United States. https://doi.org/10.1002/2016GL071353. https://www.osti.gov/servlets/purl/1465341.
@article{osti_1465341,
title = {Phase relations of Fe3C and Fe7C3 up to 185 GPa and 5200 K: Implication for the stability of iron carbide in the Earth's core},
author = {Liu, Jin and Lin, Jung-Fu and Prakapenka, Vitali B. and Prescher, Clemens and Yoshino, Takashi},
abstractNote = {We have investigated phase relations and melting behavior of Fe3C and Fe7C3 using X-ray diffraction in a laser-heated diamond cell up to 185 GPa and 5200 K. Our results show that the starting Fe3C sample decomposes into a mixture of solid orthorhombic Fe7C3 and hcp-Fe at above 145 GPa upon laser heating and then transforms into Fe-C liquid and solid Fe7C3 at temperatures above 3400 K. Using the intensity of the diffuse scattering as a primary criteria for detecting melting, the experimentally derived liquidus for a bulk composition of Fe3C fitted with the Simon-Glatzel equation is Tm(K) = 1800 × [1 + (Pm-5.7)/15.10 ± 2.55]1/2.41 ± 0.17 at 24–185 GPa, which is ~500 K higher than the melting curve of iron reported by Anzellini et al. (2013) at Earth's core pressures. The higher melting point and relative stability of Fe7C3 in Fe-rich Fe-C system at Earth's core conditions indicate that Fe7C3 could solidify out of the early Earth's molten core to become a constituent of the innermost inner core.},
doi = {10.1002/2016GL071353},
journal = {Geophysical Research Letters},
number = 24,
volume = 43,
place = {United States},
year = {Wed Dec 28 00:00:00 EST 2016},
month = {Wed Dec 28 00:00:00 EST 2016}
}

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