DOE PAGES title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Composition dependence of spin transition in (Mg,Fe)SiO3 bridgmanite

Abstract

Spin transitions in (Mg,Fe)SiO3 bridgmanite have important implications for the chemistry and dynamics of Earth’s lower mantle, but have been complex to characterize in experiments. We examine the spin state of Fe in highly Fe-enriched bridgmanite synthesized from enstatites with measured compositions (Mg0.61Fe0.38Ca0.01)SiO3 and (Mg0.25Fe0.74Ca0.01)SiO3. Bridgmanite was synthesized at 78-88 GPa and 1800-2400 K and X-ray emission spectra were measured on decompression to 1 bar (both compositions) and compression to 126 GPa ((Mg0.61Fe0.38Ca0.01)SiO3 only) without additional laser heating. Observed spectra confirm that Fe in these bridgmanites is dominantly high spin in the lower mantle. However, the total spin moment begins to decrease at ~50 GPa in the 74% FeSiO3 composition. Lastly, these results support density functional theory predictions of a lower spin transition pressure in highly Fe-enriched bridgmanite and potentially explain the high solubility of FeSiO3 in bridgmanite at pressures corresponding to Earth’s deep lower mantle.

Authors:
 [1];  [2];  [3];  [4];  [4];  [1]
  1. Ecole Polytechnique Federale de Lausanne, Lausanne (Switzerland)
  2. Ecole Polytechnique Federale de Lausanne, Lausanne (Switzerland); Univ. Paris Diderot, Paris (France)
  3. Synchrotron SOLEIL, Gif-sur-Yvette (France)
  4. Carnegie Inst. of Washington, Argonne, IL (United States)
Publication Date:
Research Org.:
Carnegie Institution of Washington, Washington, D.C. (United States)
Sponsoring Org.:
USDOE National Nuclear Security Administration (NNSA)
OSTI Identifier:
1335651
Grant/Contract Number:  
NA0002006
Resource Type:
Accepted Manuscript
Journal Name:
American Mineralogist
Additional Journal Information:
Journal Volume: 100; Journal Issue: 10; Journal ID: ISSN 0003-004X
Publisher:
Mineralogical Society of America
Country of Publication:
United States
Language:
English
Subject:
58 GEOSCIENCES; bridgmanite; spin transition; iron-bearing silicates; lower mantle

Citation Formats

Dorfman, Susannah M., Badro, James, Rueff, Jean -Pascal, Chow, Paul, Xiao, Yuming, and Gillet, Philippe. Composition dependence of spin transition in (Mg,Fe)SiO3 bridgmanite. United States: N. p., 2015. Web. doi:10.2138/am-2015-5190.
Dorfman, Susannah M., Badro, James, Rueff, Jean -Pascal, Chow, Paul, Xiao, Yuming, & Gillet, Philippe. Composition dependence of spin transition in (Mg,Fe)SiO3 bridgmanite. United States. https://doi.org/10.2138/am-2015-5190
Dorfman, Susannah M., Badro, James, Rueff, Jean -Pascal, Chow, Paul, Xiao, Yuming, and Gillet, Philippe. Thu . "Composition dependence of spin transition in (Mg,Fe)SiO3 bridgmanite". United States. https://doi.org/10.2138/am-2015-5190. https://www.osti.gov/servlets/purl/1335651.
@article{osti_1335651,
title = {Composition dependence of spin transition in (Mg,Fe)SiO3 bridgmanite},
author = {Dorfman, Susannah M. and Badro, James and Rueff, Jean -Pascal and Chow, Paul and Xiao, Yuming and Gillet, Philippe},
abstractNote = {Spin transitions in (Mg,Fe)SiO3 bridgmanite have important implications for the chemistry and dynamics of Earth’s lower mantle, but have been complex to characterize in experiments. We examine the spin state of Fe in highly Fe-enriched bridgmanite synthesized from enstatites with measured compositions (Mg0.61Fe0.38Ca0.01)SiO3 and (Mg0.25Fe0.74Ca0.01)SiO3. Bridgmanite was synthesized at 78-88 GPa and 1800-2400 K and X-ray emission spectra were measured on decompression to 1 bar (both compositions) and compression to 126 GPa ((Mg0.61Fe0.38Ca0.01)SiO3 only) without additional laser heating. Observed spectra confirm that Fe in these bridgmanites is dominantly high spin in the lower mantle. However, the total spin moment begins to decrease at ~50 GPa in the 74% FeSiO3 composition. Lastly, these results support density functional theory predictions of a lower spin transition pressure in highly Fe-enriched bridgmanite and potentially explain the high solubility of FeSiO3 in bridgmanite at pressures corresponding to Earth’s deep lower mantle.},
doi = {10.2138/am-2015-5190},
journal = {American Mineralogist},
number = 10,
volume = 100,
place = {United States},
year = {Thu Oct 01 00:00:00 EDT 2015},
month = {Thu Oct 01 00:00:00 EDT 2015}
}

Journal Article:
Free Publicly Available Full Text
Publisher's Version of Record

Citation Metrics:
Cited by: 14 works
Citation information provided by
Web of Science

Save / Share:

Works referenced in this record:

Electronic spin transitions in iron-bearing MgSiO3 perovskite
journal, January 2007

  • Stackhouse, Stephen; Brodholt, John P.; Price, G. David
  • Earth and Planetary Science Letters, Vol. 253, Issue 1-2
  • DOI: 10.1016/j.epsl.2006.10.035

Element partitioning between magnesium silicate perovskite and ferropericlase: New insights into bulk lower-mantle geochemistry
journal, May 2008

  • Auzende, Anne-Line; Badro, James; Ryerson, Frederick J.
  • Earth and Planetary Science Letters, Vol. 269, Issue 1-2
  • DOI: 10.1016/j.epsl.2008.02.001

Effect of chemistry on the compressibility of silicate perovskite in the lower mantle
journal, June 2012

  • Ballaran, Tiziana Boffa; Kurnosov, Alexander; Glazyrin, Konstantin
  • Earth and Planetary Science Letters, Vol. 333-334
  • DOI: 10.1016/j.epsl.2012.03.029

Spin and structural transitions in AlFeO3 and FeAlO3 perovskite and post-perovskite
journal, September 2010


Probing the 3d Spin Momentum with X-ray Emission Spectroscopy:  The Case of Molecular-Spin Transitions
journal, June 2006

  • Vankó, György; Neisius, Thomas; Molnár, Gábor
  • The Journal of Physical Chemistry B, Vol. 110, Issue 24
  • DOI: 10.1021/jp0615961

Partitioning of iron between perovskite/postperovskite and ferropericlase in the lower mantle
journal, January 2008

  • Sinmyo, Ryosuke; Hirose, Kei; Nishio-Hamane, Daisuke
  • Journal of Geophysical Research, Vol. 113, Issue B11
  • DOI: 10.1029/2008jb005730

Experimental evidence for the existence of iron-rich metal in the Earth's lower mantle
journal, March 2004

  • Frost, Daniel J.; Liebske, Christian; Langenhorst, Falko
  • Nature, Vol. 428, Issue 6981
  • DOI: 10.1038/nature02413

Effect of iron oxidation state on the electrical conductivity of the Earth’s lower mantle
journal, February 2013

  • Potapkin, V.; McCammon, C.; Glazyrin, K.
  • Nature Communications, Vol. 4, Issue 1
  • DOI: 10.1038/ncomms2436

Stable intermediate-spin ferrous iron in lower-mantle perovskite
journal, September 2008

  • McCammon, C.; Kantor, I.; Narygina, O.
  • Nature Geoscience, Vol. 1, Issue 10
  • DOI: 10.1038/ngeo309

Iron spin transition in Earth's mantle
journal, December 2005

  • Speziale, S.; Milner, A.; Lee, V. E.
  • Proceedings of the National Academy of Sciences, Vol. 102, Issue 50
  • DOI: 10.1073/pnas.0508919102

Spin Transition in Magnesiowüstite in Earth’s Lower Mantle
journal, May 2006


Metal-Ligand Interplay in Strongly Correlated Oxides: A Parametrized Phase Diagram for Pressure-Induced Spin Transitions
journal, May 2007


Identifying the spin transition in Fe2+-rich MgSiO3 perovskite from X-ray diffraction and vibrational spectroscopy
journal, July 2014

  • Caracas, R.; Ozawa, H.; Hirose, K.
  • American Mineralogist, Vol. 99, Issue 7
  • DOI: 10.2138/am.2014.4783

Works referencing / citing this record:

Abnormal Elasticity of Fe-Bearing Bridgmanite in the Earth's Lower Mantle
journal, May 2018

  • Fu, Suyu; Yang, Jing; Zhang, Yanyao
  • Geophysical Research Letters, Vol. 45, Issue 10
  • DOI: 10.1029/2018gl077764

First‐Principles Study of Thermodynamics and Spin Transition in FeSiO 3 Liquid at High Pressure
journal, April 2019

  • Sun, Yicheng; Zhou, Huiqun; Yin, Kun
  • Geophysical Research Letters, Vol. 46, Issue 7
  • DOI: 10.1029/2018gl081421

The GALAXIES inelastic hard X-ray scattering end-station at Synchrotron SOLEIL
journal, January 2019