Outflow of ions from Ganymede: A reinterpretation

The cold, dense plasma in the polar magnetosphere of Ganymede has been observed to contain one species of positive ions. The usual assumption that they are protons leads to severe problems, e.g. finding an adequate ionization mechanism for hydrogen, or explaining why the expected oxygen ions are not...

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Veröffentlicht in:Geophysical research letters 2000-05, Vol.27 (9), p.1347-1349
Hauptverfasser: Vasyliūnas, Vytenis M., Eviatar, Aharon
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container_title Geophysical research letters
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creator Vasyliūnas, Vytenis M.
Eviatar, Aharon
description The cold, dense plasma in the polar magnetosphere of Ganymede has been observed to contain one species of positive ions. The usual assumption that they are protons leads to severe problems, e.g. finding an adequate ionization mechanism for hydrogen, or explaining why the expected oxygen ions are not found and what happens to the oxygen. We propose that the observed ions are in fact singly charged oxygen ions rather than protons, which immediately removes all these problems. We show that the assumption of O+ instead of H+ is fully consistent with the plasma ion measurements and, by multiplying the inferred number density by 4 and speed by 1/4, brings them into better agreement with independent estimates of electron density and ion bulk flow.
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source Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; Access via Wiley Online Library; Wiley-Blackwell AGU Digital Library; Wiley Online Library (Open Access Collection)
subjects Astronomy
Earth, ocean, space
Exact sciences and technology
Ionospheres
magnetospheres
Jupiter
Planetary, asteroid, and satellite characteristics and properties
Planets, their satellites and rings. Asteroids
Solar system
title Outflow of ions from Ganymede: A reinterpretation
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