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New Simulations Undercut Giant-Impact Origin of Jupiter's Dilute Core

Peer-reviewed simulations find impacts fail to leave a lasting gradient in Jupiter's center, suggesting a gradual formation process.

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Overview

  • The study, published in Monthly Notices of the Royal Astronomical Society, reports that no simulated giant impact produced a dilute core in Jupiter.
  • Researchers used the REMIX smoothed particle hydrodynamics method on the DiRAC COSMA supercomputer with the SWIFT code to test a wide range of impact conditions and interior models.
  • Across all scenarios, heavy rock and ice displaced by impacts quickly re-settled, yielding a differentiated core with a sharp boundary rather than a smooth gradient.
  • The findings challenge earlier claims that a head-on collision by an approximately 10 Earth-mass body could create Jupiter's observed interior structure.
  • The authors note a key limitation in not modeling sub-particle chemical mixing, and they point to Saturn's similar dilute core and possible implications for interpreting gas-giant exoplanet interiors.