Estimates of Isotope Ratios in the Magnetosphere and Implications for Implantation of Atmosphere in Lunar Regolith

The plasma in Earth’s magnetosphere is comprised of ions from the solar wind and from Earth’s polar wind, with the orientation of the interplanetary magnetic field (IMF) acting to modulate the relative contributions from these two sources. Although ion composition and charge state are strong indicat...

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Main Authors: James R. Lyons, Sarah Uddin
Format: Article
Language:English
Published: MDPI AG 2025-07-01
Series:Atmosphere
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Online Access:https://www.mdpi.com/2073-4433/16/7/823
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author James R. Lyons
Sarah Uddin
author_facet James R. Lyons
Sarah Uddin
author_sort James R. Lyons
collection DOAJ
description The plasma in Earth’s magnetosphere is comprised of ions from the solar wind and from Earth’s polar wind, with the orientation of the interplanetary magnetic field (IMF) acting to modulate the relative contributions from these two sources. Although ion composition and charge state are strong indicators of ion provenance, here we consider isotope ratios as a possible additional method for tracing plasma provenance. Solar wind isotope ratios have been well characterized, but isotope ratios have not been measured for magnetospheric plasma, and only a few measurements have been made for Earth’s ionosphere. Accounting for diffusive separation in the ionosphere, and using a magnetospheric source flux model, we estimate isotope ratios for several light ions (H<sup>+</sup>, He<sup>+</sup>, N<sup>+</sup> and O<sup>+</sup>) in the magnetosphere. The primary source of N and O magnetospheric ions is the polar wind, and He ions come primarily from the solar wind. H ions come from both polar and solar winds. The extreme diffusive separation of O<sup>+</sup> isotopes argues against the polar wind as a significant source of O to the lunar regolith during the passage of the Moon through the magnetotail.
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spelling doaj-art-121990cfe84e452d923c22b66f2b726a2025-08-20T02:45:53ZengMDPI AGAtmosphere2073-44332025-07-0116782310.3390/atmos16070823Estimates of Isotope Ratios in the Magnetosphere and Implications for Implantation of Atmosphere in Lunar RegolithJames R. Lyons0Sarah Uddin1Planetary Science Institute, 1700 E. Fort Lowell, Tucson, AZ 85719, USASchool of Electrical, Computer and Energy Engineering, Arizona State University, Tempe, AZ 85287, USAThe plasma in Earth’s magnetosphere is comprised of ions from the solar wind and from Earth’s polar wind, with the orientation of the interplanetary magnetic field (IMF) acting to modulate the relative contributions from these two sources. Although ion composition and charge state are strong indicators of ion provenance, here we consider isotope ratios as a possible additional method for tracing plasma provenance. Solar wind isotope ratios have been well characterized, but isotope ratios have not been measured for magnetospheric plasma, and only a few measurements have been made for Earth’s ionosphere. Accounting for diffusive separation in the ionosphere, and using a magnetospheric source flux model, we estimate isotope ratios for several light ions (H<sup>+</sup>, He<sup>+</sup>, N<sup>+</sup> and O<sup>+</sup>) in the magnetosphere. The primary source of N and O magnetospheric ions is the polar wind, and He ions come primarily from the solar wind. H ions come from both polar and solar winds. The extreme diffusive separation of O<sup>+</sup> isotopes argues against the polar wind as a significant source of O to the lunar regolith during the passage of the Moon through the magnetotail.https://www.mdpi.com/2073-4433/16/7/823isotopesionospheremagnetospheresolar windpolar windlunar regolith
spellingShingle James R. Lyons
Sarah Uddin
Estimates of Isotope Ratios in the Magnetosphere and Implications for Implantation of Atmosphere in Lunar Regolith
Atmosphere
isotopes
ionosphere
magnetosphere
solar wind
polar wind
lunar regolith
title Estimates of Isotope Ratios in the Magnetosphere and Implications for Implantation of Atmosphere in Lunar Regolith
title_full Estimates of Isotope Ratios in the Magnetosphere and Implications for Implantation of Atmosphere in Lunar Regolith
title_fullStr Estimates of Isotope Ratios in the Magnetosphere and Implications for Implantation of Atmosphere in Lunar Regolith
title_full_unstemmed Estimates of Isotope Ratios in the Magnetosphere and Implications for Implantation of Atmosphere in Lunar Regolith
title_short Estimates of Isotope Ratios in the Magnetosphere and Implications for Implantation of Atmosphere in Lunar Regolith
title_sort estimates of isotope ratios in the magnetosphere and implications for implantation of atmosphere in lunar regolith
topic isotopes
ionosphere
magnetosphere
solar wind
polar wind
lunar regolith
url https://www.mdpi.com/2073-4433/16/7/823
work_keys_str_mv AT jamesrlyons estimatesofisotoperatiosinthemagnetosphereandimplicationsforimplantationofatmosphereinlunarregolith
AT sarahuddin estimatesofisotoperatiosinthemagnetosphereandimplicationsforimplantationofatmosphereinlunarregolith