Ejected Particles after Impact Splash on Mars: Aggregates and Aerodynamics
Our earlier laboratory measurements showed that low-velocity sand impacts release fine <5 μ m dust from a Martian simulant soil. This dust will become airborne in the Martian atmosphere. Here, we extend this study by measuring aerodynamic properties of ejecta and characterizing deviations from the b...
I tiakina i:
| Ngā kaituhi matua: | , , , , , , , , |
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| Hōputu: | Artigo |
| Reo: | Inglês |
| I whakaputaina: |
IOP Publishing
2023-01-01
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| Rangatū: | The Planetary Science Journal |
| Ngā marau: | |
| Urunga tuihono: | https://doi.org/10.3847/PSJ/acf318 |
| Ngā Tūtohu: |
Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!
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