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Depth-dependent anisotropy in the Earth’s inner core linked to chemical stratification

Author

Listed:
  • Efim Kolesnikov

    (University of Münster, Institute for Mineralogy
    UMR 8207 - UMET - Unité Matériaux et Transformations, Univ. Lille, CNRS, INRAE, Centrale Lille)

  • Xiang Li

    (University of Münster, Institute for Mineralogy
    The European Synchrotron, ESRF)

  • Susanne C. Müller

    (University of Münster, Institute for Mineralogy
    The European Synchrotron, ESRF)

  • Arno Rohrbach

    (University of Münster, Institute for Mineralogy)

  • Stephan Klemme

    (University of Münster, Institute for Mineralogy)

  • Jasper Berndt

    (University of Münster, Institute for Mineralogy)

  • Hanns-Peter Liermann

    (Deutsches Elektronen-Synchrotron DESY)

  • Carmen Sanchez-Valle

    (University of Münster, Institute for Mineralogy)

  • Ilya Kupenko

    (University of Münster, Institute for Mineralogy
    The European Synchrotron, ESRF)

Abstract

Seismic anisotropy in the Earth’s inner core (IC), including the heterogeneous, depth-dependent anisotropy structure, is a well-documented yet poorly understood feature plausibly related to the alignment of iron alloy crystals. Here, we report the effect of silicon and carbon on the plastic deformation of hexagonal close-packed (hcp) iron using radial X-ray diffraction at pressures up to 128 GPa and temperatures up to 1100 K. Our results reveal a low compressional wave anisotropy (~2 %) in the Fe-Si-C alloy, consistent with the seismic anisotropy observed in the outer regions of the IC. These findings, together with the higher anisotropy exhibited by pure hcp-Fe, suggest that the depth-dependent elastic anisotropy of the IC may originate from chemical stratification, i.e., radial gradients in silicon and carbon concentrations, during crystallization.

Suggested Citation

  • Efim Kolesnikov & Xiang Li & Susanne C. Müller & Arno Rohrbach & Stephan Klemme & Jasper Berndt & Hanns-Peter Liermann & Carmen Sanchez-Valle & Ilya Kupenko, 2025. "Depth-dependent anisotropy in the Earth’s inner core linked to chemical stratification," Nature Communications, Nature, vol. 16(1), pages 1-11, December.
  • Handle: RePEc:nat:natcom:v:16:y:2025:i:1:d:10.1038_s41467-025-67067-y
    DOI: 10.1038/s41467-025-67067-y
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