Journal Article PUBDB-2025-05569

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

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2025
Springer Nature [London]

Nature Communications 16, 10986 () [10.1038/s41467-025-67067-y]
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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.

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Note: The grant from German ResearchFoundation (DFG) through the DFG Project AOBJ: 662965 GZ.:KU 3832/2–1 was not found in the system. Please add this one also to the financial sources

Contributing Institute(s):
  1. DOOR-User (DOOR ; HAS-User)
  2. Experimentebetreuung PETRA III (FS-PET-D)
Research Program(s):
  1. 631 - Matter – Dynamics, Mechanisms and Control (POF4-631) (POF4-631)
  2. 6G3 - PETRA III (DESY) (POF4-6G3) (POF4-6G3)
  3. FS-Proposal: I-20211268 (I-20211268) (I-20211268)
  4. LECOR - Light elements in the core (101042572) (101042572)
Experiment(s):
  1. PETRA Beamline P02.2 (PETRA III)

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 Record created 2025-12-15, last modified 2026-01-09


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