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Updated: Feb 7, 2026

Visualization of Failure and the Associated Grain-Scale Mechanical Behavior of Granular Soils under Shear using Synchrotron X-Ray Micro-Tomography
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Ray Systems in Granular Cratering.

Tapan Sabuwala1, Christian Butcher2, Gustavo Gioia1

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Summary
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Surface undulations transform ejecta blankets into ray systems during granular cratering. The number of rays correlates with impactor size and surface wavelength, offering insights into planetary cratering.

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Area of Science:

  • Planetary Science
  • Geophysics
  • Fluid Dynamics

Background:

  • Classical granular cratering experiments yield uniform ejecta blankets.
  • The influence of surface topography on ejecta patterns has been largely unaddressed.

Purpose of the Study:

  • To investigate how surface undulations affect ejecta patterns in granular cratering.
  • To understand the formation mechanism of rayed crater systems.

Main Methods:

  • Conducted numerous granular cratering experiments.
  • Performed computational simulations of the cratering process.
  • Analyzed the relationship between impactor size, surface wavelength, and ray system characteristics.

Main Results:

  • Surface undulations transform uniform ejecta blankets into ray systems.
  • The number of rays in a ray system is directly proportional to the impactor diameter (D) and inversely proportional to the surface undulation wavelength (λ).
  • Ejecta forming ray systems originate from a narrow annular region around the impact site.

Conclusions:

  • Surface topography is a critical factor in determining ejecta patterns.
  • The findings provide a physical model for the formation of rayed craters observed on planetary bodies.
  • This research may help explain enigmatic ray systems on the Moon and other celestial bodies.