Magnetic transition and sound velocities of Fe3S at high pressure:: implications for Earth and planetary cores

被引:57
|
作者
Lin, JF
Fei, YW
Sturhahn, W
Zhao, JY
Mao, HK
Hemley, RJ
机构
[1] Carnegie Inst Sci, Geophys Lab, Washington, DC 20015 USA
[2] Argonne Natl Lab, Adv Photon Source, Argonne, IL 60439 USA
基金
美国国家科学基金会; 美国国家航空航天局;
关键词
light element; sound velocity; Fe3S; Earth's core; sulfur;
D O I
10.1016/j.epsl.2004.07.018
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Magnetic, elastic, thermodynamic, and vibrational properties of the most iron-rich sulfide, Fe3S, known to date have been studied with synchrotron Mossbauer spectroscopy (SMS) and nuclear resonant inelastic X-ray scattering (NRIXS) up to 57 GPa at room temperature. The magnetic hyperfine fields derived from the time spectra of the synchrotron Mossbauer spectroscopy show that the low-pressure magnetic phase displays two magnetic hyperfine field sites and that a magnetic collapse occurs at 21 GPa. The magnetic to non-magnetic transition significantly affects the elastic, thermodynamic, and vibrational properties of Fe3S. The magnetic collapse of Fe3S may also affect the phase relations in the iron-sulfur system, changing the solubility of sulfur in iron under higher pressures. Determination of the physical properties of the nonmagnetic Fe3S phase is important for the interpretation of the amount and properties of sulfur present in the planetary cores. Sound velocities of Fe3S obtained from the measured partial phonon density of states (PDOS) for Fe-57 incorporated in the alloy show that Fe3S has higher compressional and shear wave velocity than those of hcp-Fe and hcp-Fe0.92Ni0.08 alloy under high pressures, making sulfur a potential light element in the Earth's core based on geophysical arguments. The V-P and V-S of the non-magnetic Fe3S follow a Birch's law trend whereas the slopes decrease in the magnetic phase, indicating that the decrease of the magnetic moment significantly affects the sound velocities. If the Martian core is in the solid state containing 14.2 wt.% sulfur, it is likely that the non-magnetic Fe3S phase is a dominant component and that our measured sound velocities of Fe3S can be used to construct the corresponding velocity profile of the Martian core. It is also conceivable that Fe3P and Fe3C undergo similar magnetic phase transitions under high pressures. (C) 2004 Elsevier B.V. All rights reserved.
引用
收藏
页码:33 / 40
页数:8
相关论文
共 50 条
  • [1] Ab initio study of structural, elastic and thermodynamic properties of Fe3S at high pressure: Implications for planetary cores
    Valencia, Karen
    De Moya, Aldemar
    Morard, Guillaume
    Allan, Neil L.
    Pinilla, Carlos
    AMERICAN MINERALOGIST, 2022, 107 (02) : 248 - 256
  • [2] Pressure-induced magnetic transition and sound velocities of Fe3C:: Implications for carbon in the Earth's inner core
    Gao, Lili
    Chen, Bin
    Wang, Jingyun
    Alp, Esen E.
    Zhao, Jiyong
    Lerche, Michael
    Sturhahn, Wolfgang
    Scott, Henry P.
    Huang, Fang
    Ding, Yang
    Sinogeikin, Stanislav V.
    Lundstrom, Craig C.
    Bass, Jay D.
    Li, Jie
    GEOPHYSICAL RESEARCH LETTERS, 2008, 35 (17)
  • [3] Sound wave velocities of Fe5Si at high-pressure and high-temperature conditions: Implications to lunar and planetary cores
    Deng, Liwei
    Kono, Yoshio
    Shen, Guoyin
    AMERICAN MINERALOGIST, 2019, 104 (02) : 291 - 299
  • [4] Sound velocity measurements in liquid Fe-S at high pressure: Implications for Earth's and lunar cores
    Nishida, Keisuke
    Kono, Yoshio
    Terasaki, Hidenori
    Takahashi, Suguru
    Ishii, Miho
    Shimoyama, Yuta
    Higo, Yuji
    Funakoshi, Ken-ichi
    Irifune, Tetsuo
    Ohtani, Eiji
    EARTH AND PLANETARY SCIENCE LETTERS, 2013, 362 : 182 - 186
  • [5] The sound velocity measurements of Fe3S
    Kamada, Seiji
    Ohtani, Eiji
    Fukui, Hiroshi
    Sakai, Takeshi
    Terasaki, Hidenori
    Takahashi, Suguru
    Shibazaki, Yuki
    Tsutsui, Satoshi
    Baron, Alfred Q. R.
    Hirao, Naohisa
    Ohishi, Yasuo
    AMERICAN MINERALOGIST, 2014, 99 (01) : 98 - 101
  • [6] High-pressure melting experiments of Fe3S and a thermodynamic model of the Fe-S liquids for the Earth's core
    Thompson, Samuel
    Sugimura-Komabayashi, Emiko
    Komabayashi, Tetsuya
    McGuire, Chris
    Breton, Helene
    Suehiro, Sho
    Ohishi, Yasuo
    JOURNAL OF PHYSICS-CONDENSED MATTER, 2022, 34 (39)
  • [7] Thermal equation of state of Fe3S and implications for sulfur in Earth's core
    Seagle, Christopher T.
    Campbell, Andrew J.
    Heinz, Dion L.
    Shen, Guoyin
    Prakapenka, Vitali B.
    JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2006, 111 (B6)
  • [8] Immiscible two-liquid regions in the Fe-O-S system at high pressure: Implications for planetary cores
    Tsuno, Kyusei
    Ohtani, Eiji
    Terasaki, Hidenori
    PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 2007, 160 (01) : 75 - 85
  • [9] High-pressure melting relations in Fe-C-S systems: Implications for metallic cores in planetary bodies
    Dasgupta, R.
    Whelan, G.
    Buono, A.
    Walker, D.
    GEOCHIMICA ET COSMOCHIMICA ACTA, 2008, 72 (12) : A199 - A199
  • [10] Sound velocities of Fe and Fe-Si alloy in the Earth's core
    Mao, Zhu
    Lin, Jung-Fu
    Liu, Jin
    Alatas, Ahmet
    Gao, Lili
    Zhao, Jiyong
    Mao, Ho-Kwang
    PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2012, 109 (26) : 10239 - 10244