Direct observations of negative ions on the Lunar surface by Chang'E-6

Abstract The solar wind can interact directly with the surface of airless bodies like the Moon. The interaction causes sputtering of surface materials and solar wind ions are also partially backscattered to space. Particles leaving the surface can have any charge-state. At the Moon, backscattered or...

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Main Authors: Martin Wieser, Aibing Zhang, Romain Canu-Blot, Wengjing Wang, Gabriella Stenberg Wieser, Lianghai Xie, Stas Barabash, Tianhua Zhong, Xiao-Dong Wang, Yongliao Zou, Máté Kerényi, Weibin Wen, Charles Lue, Chi Wang
Format: Article
Language:English
Published: Nature Portfolio 2025-06-01
Series:Communications Earth & Environment
Online Access:https://doi.org/10.1038/s43247-025-02399-7
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author Martin Wieser
Aibing Zhang
Romain Canu-Blot
Wengjing Wang
Gabriella Stenberg Wieser
Lianghai Xie
Stas Barabash
Tianhua Zhong
Xiao-Dong Wang
Yongliao Zou
Máté Kerényi
Weibin Wen
Charles Lue
Chi Wang
author_facet Martin Wieser
Aibing Zhang
Romain Canu-Blot
Wengjing Wang
Gabriella Stenberg Wieser
Lianghai Xie
Stas Barabash
Tianhua Zhong
Xiao-Dong Wang
Yongliao Zou
Máté Kerényi
Weibin Wen
Charles Lue
Chi Wang
author_sort Martin Wieser
collection DOAJ
description Abstract The solar wind can interact directly with the surface of airless bodies like the Moon. The interaction causes sputtering of surface materials and solar wind ions are also partially backscattered to space. Particles leaving the surface can have any charge-state. At the Moon, backscattered or sputtered positive ions1–4 and energetic neutral atoms5–8 have been observed, but all attempts to find negative ions in electron measurements have failed so far. Here we present measurements by Chang’E-6 from the lunar farside9 revealing the existence of a layer of negative ions close to the lunar surface. We found that about $$2.{5}_{-0.8}^{+1.2} \%$$ 2 . 5 − 0.8 + 1.2 % of the impinging solar wind protons charge exchange on the lunar regolith and are backscattered as negative hydrogen ions. The negative ion fraction is similar to the observed positive ion fraction1,3. We estimate a H− surface density of $$0.1{8}_{-0.03}^{+0.04}\,{{{{\rm{cm}}}}}^{-3}$$ 0.1 8 − 0.03 + 0.04 cm − 3 . On the dayside, the lifetime of negative hydrogen ions is short due to photodetachment10, confining them to a layer with a scale height of about 10 km. Such surface-bound layers or regions with negative ions should exist at any planetary object with a surface directly exposed to solar wind11,12, including low gravity bodies such as asteroids or comets.
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spelling doaj-art-9879ad0822ff40dca2d982645e6f4e4d2025-08-20T03:21:06ZengNature PortfolioCommunications Earth & Environment2662-44352025-06-016111010.1038/s43247-025-02399-7Direct observations of negative ions on the Lunar surface by Chang'E-6Martin Wieser0Aibing Zhang1Romain Canu-Blot2Wengjing Wang3Gabriella Stenberg Wieser4Lianghai Xie5Stas Barabash6Tianhua Zhong7Xiao-Dong Wang8Yongliao Zou9Máté Kerényi10Weibin Wen11Charles Lue12Chi Wang13Swedish Institute of Space Physics (IRF)National Space Science Center (NSSC), Chinese Academy of Sciences (CAS)Swedish Institute of Space Physics (IRF)National Space Science Center (NSSC), Chinese Academy of Sciences (CAS)Swedish Institute of Space Physics (IRF)National Space Science Center (NSSC), Chinese Academy of Sciences (CAS)Swedish Institute of Space Physics (IRF)National Space Science Center (NSSC), Chinese Academy of Sciences (CAS)Swedish Institute of Space Physics (IRF)National Space Science Center (NSSC), Chinese Academy of Sciences (CAS)Swedish Institute of Space Physics (IRF)National Astronomical Observatories, Chinese Academy of SciencesSwedish Institute of Space Physics (IRF)National Space Science Center (NSSC), Chinese Academy of Sciences (CAS)Abstract The solar wind can interact directly with the surface of airless bodies like the Moon. The interaction causes sputtering of surface materials and solar wind ions are also partially backscattered to space. Particles leaving the surface can have any charge-state. At the Moon, backscattered or sputtered positive ions1–4 and energetic neutral atoms5–8 have been observed, but all attempts to find negative ions in electron measurements have failed so far. Here we present measurements by Chang’E-6 from the lunar farside9 revealing the existence of a layer of negative ions close to the lunar surface. We found that about $$2.{5}_{-0.8}^{+1.2} \%$$ 2 . 5 − 0.8 + 1.2 % of the impinging solar wind protons charge exchange on the lunar regolith and are backscattered as negative hydrogen ions. The negative ion fraction is similar to the observed positive ion fraction1,3. We estimate a H− surface density of $$0.1{8}_{-0.03}^{+0.04}\,{{{{\rm{cm}}}}}^{-3}$$ 0.1 8 − 0.03 + 0.04 cm − 3 . On the dayside, the lifetime of negative hydrogen ions is short due to photodetachment10, confining them to a layer with a scale height of about 10 km. Such surface-bound layers or regions with negative ions should exist at any planetary object with a surface directly exposed to solar wind11,12, including low gravity bodies such as asteroids or comets.https://doi.org/10.1038/s43247-025-02399-7
spellingShingle Martin Wieser
Aibing Zhang
Romain Canu-Blot
Wengjing Wang
Gabriella Stenberg Wieser
Lianghai Xie
Stas Barabash
Tianhua Zhong
Xiao-Dong Wang
Yongliao Zou
Máté Kerényi
Weibin Wen
Charles Lue
Chi Wang
Direct observations of negative ions on the Lunar surface by Chang'E-6
Communications Earth & Environment
title Direct observations of negative ions on the Lunar surface by Chang'E-6
title_full Direct observations of negative ions on the Lunar surface by Chang'E-6
title_fullStr Direct observations of negative ions on the Lunar surface by Chang'E-6
title_full_unstemmed Direct observations of negative ions on the Lunar surface by Chang'E-6
title_short Direct observations of negative ions on the Lunar surface by Chang'E-6
title_sort direct observations of negative ions on the lunar surface by chang e 6
url https://doi.org/10.1038/s43247-025-02399-7
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