Cassini Finds an Oxygen-Carbon Dioxide Atmosphere at Saturn's Icy Moon Rhea
The flyby measurements of the Cassini spacecraft at Saturn's moon Rhea reveal a tenuous oxygen (O₂)-carbon dioxide (CO₂) atmosphere. The atmosphere appears to be sustained by chemical decomposition of the surface water ice under irradiation from Saturn's magnetospheric plasma. This in situ...
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Veröffentlicht in: | Science (American Association for the Advancement of Science) 2010-12, Vol.330 (6012), p.1813-1815 |
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creator | Teolis, B.D Jones, G.H Miles, P.F Tokar, R.L Magee, B.A Waite, J.H Roussos, E Young, D.T Crary, F.J Coates, A.J Johnson, R.E Tseng, W.-L Baragiola, R.A |
description | The flyby measurements of the Cassini spacecraft at Saturn's moon Rhea reveal a tenuous oxygen (O₂)-carbon dioxide (CO₂) atmosphere. The atmosphere appears to be sustained by chemical decomposition of the surface water ice under irradiation from Saturn's magnetospheric plasma. This in situ detection of an oxidizing atmosphere is consistent with remote observations of other icy bodies, such as Jupiter's moons Europa and Ganymede, and suggestive of a reservoir of radiolytic O₂ locked within Rhea's ice. The presence of CO₂ suggests radiolysis reactions between surface oxidants and organics or sputtering and/or outgassing of CO₂ endogenic to Rhea's ice. Observations of outflowing positive and negative ions give evidence for pickup ionization as a major atmospheric loss mechanism. |
doi_str_mv | 10.1126/science.1198366 |
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The atmosphere appears to be sustained by chemical decomposition of the surface water ice under irradiation from Saturn's magnetospheric plasma. This in situ detection of an oxidizing atmosphere is consistent with remote observations of other icy bodies, such as Jupiter's moons Europa and Ganymede, and suggestive of a reservoir of radiolytic O₂ locked within Rhea's ice. The presence of CO₂ suggests radiolysis reactions between surface oxidants and organics or sputtering and/or outgassing of CO₂ endogenic to Rhea's ice. 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The atmosphere appears to be sustained by chemical decomposition of the surface water ice under irradiation from Saturn's magnetospheric plasma. This in situ detection of an oxidizing atmosphere is consistent with remote observations of other icy bodies, such as Jupiter's moons Europa and Ganymede, and suggestive of a reservoir of radiolytic O₂ locked within Rhea's ice. The presence of CO₂ suggests radiolysis reactions between surface oxidants and organics or sputtering and/or outgassing of CO₂ endogenic to Rhea's ice. Observations of outflowing positive and negative ions give evidence for pickup ionization as a major atmospheric loss mechanism.</description><subject>Astronomy</subject><subject>Atmosphere</subject><subject>Atmospherics</subject><subject>Carbon Dioxide</subject><subject>Chemical composition</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Extraterrestrial Environment</subject><subject>Galilean satellites</subject><subject>Hemispheres</subject><subject>Ice</subject><subject>Ions</subject><subject>Jupiter</subject><subject>Mass Spectrometry</subject><subject>Molecules</subject><subject>Moons</subject><subject>Natural satellites</subject><subject>Oxygen</subject><subject>Photochemical Processes</subject><subject>Planetary, asteroid, and satellite characteristics and properties</subject><subject>Planets, their satellites and rings. 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subjects | Astronomy Atmosphere Atmospherics Carbon Dioxide Chemical composition Earth, ocean, space Exact sciences and technology Extraterrestrial Environment Galilean satellites Hemispheres Ice Ions Jupiter Mass Spectrometry Molecules Moons Natural satellites Oxygen Photochemical Processes Planetary, asteroid, and satellite characteristics and properties Planets, their satellites and rings. Asteroids Saturn Saturnian satellites Solar system Spacecraft Trajectories |
title | Cassini Finds an Oxygen-Carbon Dioxide Atmosphere at Saturn's Icy Moon Rhea |
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