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Title: Seismic parameters of hcp‐Fe alloyed with Ni and Si in the Earth's inner core

Abstract

Abstract Iron alloyed with Ni and Si has been suggested to be a major component of the Earth's inner core. High‐pressure results on the combined alloying effects of Ni and Si on seismic parameters of iron are thus essential for establishing satisfactory geophysical and geochemical models of the region. Here we have investigated the compressional ( V P ) and shear ( Vs ) wave velocity‐density ( ρ ) relations, Poisson's ratio ( ν ), and seismic heterogeneity ratios ( dlnρ / dlnV P , dlnρ / dlnV S , and dlnV P / dlnV S ) of hcp‐Fe and hcp‐Fe 86.8 Ni 8.6 Si 4.6 alloy up to 206 GPa and 136 GPa, respectively, using multiple complementary techniques. Compared with the literature velocity values for hcp‐Fe and Fe‐Ni‐Si alloys, our results show that the combined addition of 9.0 wt % Ni and 2.3 wt % Si slightly increases the V P but significantly decreases the V S of hcp‐Fe at a given density relevant to the inner core. Such distinct alloying effects on velocities of hcp‐Fe produce a high ν of about 0.40 for the alloy at inner core densities, which is approximately 20% higher than that for hcp‐Fe. Analysis of the literature high P‐Tmore » results on V P and V S of Fe alloyed with light elements shows that high temperature can further enhance the ν of hcp‐Fe alloyed with Ni and Si. Most significantly, the derived seismic heterogeneity ratios of this hcp alloy present a better match with global seismic observations. Our results provide a multifactored geophysical constraint on the compositional model of the inner core which is consistent with silicon being a major light element alloyed with Fe and 5 wt % Ni.« less

Authors:
 [1];  [2];  [3];  [3];  [3];  [4]
  1. Department of Geological Sciences, Jackson School of Geosciences University of Texas at Austin Austin Texas USA
  2. Department of Geological Sciences, Jackson School of Geosciences University of Texas at Austin Austin Texas USA, Center for High Pressure Science and Advanced Technology Research Shanghai China
  3. Advanced Photon Source Argonne National Laboratory Argonne Illinois USA
  4. Bayerisches Geoinstitut Universität Bayreuth Bayreuth Germany
Publication Date:
Sponsoring Org.:
USDOE
OSTI Identifier:
1402160
Resource Type:
Publisher's Accepted Manuscript
Journal Name:
Journal of Geophysical Research. Solid Earth
Additional Journal Information:
Journal Name: Journal of Geophysical Research. Solid Earth Journal Volume: 121 Journal Issue: 2; Journal ID: ISSN 2169-9313
Publisher:
American Geophysical Union (AGU)
Country of Publication:
United States
Language:
English

Citation Formats

Liu, Jin, Lin, Jung‐Fu, Alatas, Ahmet, Hu, Michael Y., Zhao, Jiyong, and Dubrovinsky, Leonid. Seismic parameters of hcp‐Fe alloyed with Ni and Si in the Earth's inner core. United States: N. p., 2016. Web. doi:10.1002/2015JB012625.
Liu, Jin, Lin, Jung‐Fu, Alatas, Ahmet, Hu, Michael Y., Zhao, Jiyong, & Dubrovinsky, Leonid. Seismic parameters of hcp‐Fe alloyed with Ni and Si in the Earth's inner core. United States. https://doi.org/10.1002/2015JB012625
Liu, Jin, Lin, Jung‐Fu, Alatas, Ahmet, Hu, Michael Y., Zhao, Jiyong, and Dubrovinsky, Leonid. Thu . "Seismic parameters of hcp‐Fe alloyed with Ni and Si in the Earth's inner core". United States. https://doi.org/10.1002/2015JB012625.
@article{osti_1402160,
title = {Seismic parameters of hcp‐Fe alloyed with Ni and Si in the Earth's inner core},
author = {Liu, Jin and Lin, Jung‐Fu and Alatas, Ahmet and Hu, Michael Y. and Zhao, Jiyong and Dubrovinsky, Leonid},
abstractNote = {Abstract Iron alloyed with Ni and Si has been suggested to be a major component of the Earth's inner core. High‐pressure results on the combined alloying effects of Ni and Si on seismic parameters of iron are thus essential for establishing satisfactory geophysical and geochemical models of the region. Here we have investigated the compressional ( V P ) and shear ( Vs ) wave velocity‐density ( ρ ) relations, Poisson's ratio ( ν ), and seismic heterogeneity ratios ( dlnρ / dlnV P , dlnρ / dlnV S , and dlnV P / dlnV S ) of hcp‐Fe and hcp‐Fe 86.8 Ni 8.6 Si 4.6 alloy up to 206 GPa and 136 GPa, respectively, using multiple complementary techniques. Compared with the literature velocity values for hcp‐Fe and Fe‐Ni‐Si alloys, our results show that the combined addition of 9.0 wt % Ni and 2.3 wt % Si slightly increases the V P but significantly decreases the V S of hcp‐Fe at a given density relevant to the inner core. Such distinct alloying effects on velocities of hcp‐Fe produce a high ν of about 0.40 for the alloy at inner core densities, which is approximately 20% higher than that for hcp‐Fe. Analysis of the literature high P‐T results on V P and V S of Fe alloyed with light elements shows that high temperature can further enhance the ν of hcp‐Fe alloyed with Ni and Si. Most significantly, the derived seismic heterogeneity ratios of this hcp alloy present a better match with global seismic observations. Our results provide a multifactored geophysical constraint on the compositional model of the inner core which is consistent with silicon being a major light element alloyed with Fe and 5 wt % Ni.},
doi = {10.1002/2015JB012625},
journal = {Journal of Geophysical Research. Solid Earth},
number = 2,
volume = 121,
place = {United States},
year = {Thu Feb 18 00:00:00 EST 2016},
month = {Thu Feb 18 00:00:00 EST 2016}
}

Journal Article:
Free Publicly Available Full Text
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https://doi.org/10.1002/2015JB012625

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Cited by: 12 works
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