Deducing Lunar Regolith Porosity From Energetic Neutral Atom Emission

Szabo, P. S.; Poppe, A. R.; Biber, H.; Mutzke, A.; Pichler, J.; Jäggi, N.; Galli, A.; Wurz, P.; Aumayr, F. (2022). Deducing Lunar Regolith Porosity From Energetic Neutral Atom Emission. Geophysical Research Letters, 49(21) American Geophysical Union 10.1029/2022gl101232

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The porosity of the upper layers of regolith is key to the interaction of an airless planetary body with precipitating radiation, but it remains difficult to characterize. One of the effects that is governed by regolith properties is Energetic Neutral Atom (ENA) emission in the form of reflected and neutralized solar wind protons. We simulate this process for the surface of the Moon by implementing a regolith grain stacking in the ion-solid-interaction software SDTrimSP-3D, finding that proton reflection significantly depends on the regolith porosity. Via comparison with ENA measurements by Chandrayaan-1, we derive a globally averaged porosity of the uppermost regolith layers of urn:x-wiley:00948276:media:grl65047:grl65047-math-0001. These results indicate a highly porous, fairy-castle-like nature of the upper lunar regolith, as well as its importance for the interaction with impacting ions. Our simulations further outline the possibility of future regolith studies with ENA measurements, for example, by the BepiColombo mission to Mercury.

Item Type:

Journal Article (Original Article)

Division/Institute:

08 Faculty of Science > Physics Institute > Space Research and Planetary Sciences
08 Faculty of Science > Physics Institute

UniBE Contributor:

Jäggi, Noah Victor, Galli, A, Wurz, Peter

Subjects:

500 Science > 530 Physics
500 Science > 520 Astronomy
600 Technology > 620 Engineering

ISSN:

0094-8276

Publisher:

American Geophysical Union

Language:

English

Submitter:

Dora Ursula Zimmerer

Date Deposited:

10 Mar 2023 13:37

Last Modified:

18 May 2023 00:25

Publisher DOI:

10.1029/2022gl101232

BORIS DOI:

10.48350/179771

URI:

https://boris.unibe.ch/id/eprint/179771

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