Dusty streaks on the Moon: fingerprints of multiphase flow instabilities

From the crewed Apollo missions to the recent Chinese Chang'e landings, the interaction between spacecraft exhaust plumes and lunar soil produces dusty clouds with high-speed particle ejection. Despite varying landing sites, remarkably stable streak patterns were observed, raising questions about their origin. We solved this puzzle by showing that these patterns were driven by Görtler instability from the curved compressed shear layer of the supersonic but surprisingly laminar jet. This instability creates vortical structures that entrain and eject particles. The number of streaks exhibits an interesting scaling with the jet pressure ratio, which can be modeled with linear instability theory and shows excellent agreement with scaled-down experiments, simulations, and actual observations in landing videos. Our findings provide a fluid physics explanation of extraterrestrial landings, highlighting the role of particle-laden flows and paving the way for future missions to optimize landing strategies and mitigate dust cloud effects on equipment and visibility.

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Publication Details

Journal
Nature Communications
Published
2025-07-19
DOI
https://doi.org/10.1038/s41467-025-62001-8
Citations
3
Primary Topic
Particle Dynamics in Fluid Flows
Type
article
Field-Weighted Citation Impact
3.44

Funders

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article

Dusty streaks on the Moon: fingerprints of multiphase flow instabilities

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3 citations
Nature Communications
Particle Dynamics in Fluid Flows
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article

Dusty streaks on the Moon: fingerprints of multiphase flow instabilities

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article en
3 citations

Abstract

From the crewed Apollo missions to the recent Chinese Chang'e landings, the interaction between spacecraft exhaust plumes and lunar soil produces dusty clouds with high-speed particle ejection. Despite varying landing sites, remarkably stable streak patterns were observed, raising questions about their origin. We solved this puzzle by showing that these patterns were driven by Görtler instability from the curved compressed shear layer of the supersonic but surprisingly laminar jet. This instability creates vortical structures that entrain and eject particles. The number of streaks exhibits an interesting scaling with the jet pressure ratio, which can be modeled with linear instability theory and shows excellent agreement with scaled-down experiments, simulations, and actual observations in landing videos. Our findings provide a fluid physics explanation of extraterrestrial landings, highlighting the role of particle-laden flows and paving the way for future missions to optimize landing strategies and mitigate dust cloud effects on equipment and visibility.

Nature CommunicationsVol. 16(1)
Langley Research Center (US), Johns Hopkins University (US), University of Michigan (US)
National Aeronautics and Space Administration, Nuclear Safety and Security Commission, Marshall Space Flight Center, Langley Research Center, Space Technology Mission Directorate
Openalex Percentile: Top 8%
Particle Dynamics in Fluid Flows
3.44
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