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On the origins of backscattered solar wind energetic neutral hydrogen from the Moon and Mercury
The surfaces of planetary airless bodies are directly bombarded by solar particles. The most abundant of those particles are solar wind protons. In the case of the Moon, many in situ observations have shown that a significant portion of these incident solar-wind protons are backscattered as energeti...
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Published in: | Planetary and space science 2023-05, Vol.229, p.105660, Article 105660 |
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Main Authors: | , , , , , , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | The surfaces of planetary airless bodies are directly bombarded by solar particles. The most abundant of those particles are solar wind protons. In the case of the Moon, many in situ observations have shown that a significant portion of these incident solar-wind protons are backscattered as energetic neutral hydrogen atoms (ENA). Measurements of the energy flux distribution of these neutral particles provide a clue regarding the processes occurring in the surface regolith when impacting protons collide with the surface grains.
In this work, we developed a model to describe the fate of protons through a regolith model and compared our results with Chandrayaan-1 ENA measurements. We combined a Monte Carlo approach to reconstruct the motion of these particles into a layer of grains with molecular dynamics to parametrize the interaction of an incident proton with a grain. Using simultaneous measurements of the incident plasma by Chandrayaan-1 SWIM, this detailed modelling allowed us to analyse the measurements performed by the Chandrayaan-1 CENA instrument when the Moon is in the solar wind and in the Earth's magnetosheath, and to highlight what could control the flux and energy properties of these backscattered neutral hydrogen particles. Predictions of the intensity and shape of the backscattered neutral hydrogen distribution at Mercury are derived from this calculation.
•The Moon surface is a very efficient backscattering surface for incident Solar Wind protons.•How much protons are really backscattered and with which energy remain debated.•We model the fate of incident protons into a regolith.•We here show how some parameters might impact the backscattered energy flux.•We also make some predictions of the backscattered flux of protons at Mercury. |
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ISSN: | 0032-0633 1873-5088 |
DOI: | 10.1016/j.pss.2023.105660 |