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In situ collection of dust grains falling from Saturn's rings into its atmosphere
Saturn's main rings are composed of >95% water ice, and the nature of the remaining few percent has remained unclear. The Cassini spacecraft's traversals between Saturn and its innermost D ring allowed its cosmic dust analyzer (CDA) to collect material released from the main rings and t...
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Published in: | Science (American Association for the Advancement of Science) 2018-10, Vol.362 (6410) |
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creator | Hsu, Hsiang-Wen Schmidt, Jürgen Kempf, Sascha Postberg, Frank Moragas-Klostermeyer, Georg Seiß, Martin Hoffmann, Holger Burton, Marcia Ye, ShengYi Kurth, William S Horányi, Mihály Khawaja, Nozair Spahn, Frank Schirdewahn, Daniel O'Donoghue, James Moore, Luke Cuzzi, Jeff Jones, Geraint H Srama, Ralf |
description | Saturn's main rings are composed of >95% water ice, and the nature of the remaining few percent has remained unclear. The Cassini spacecraft's traversals between Saturn and its innermost D ring allowed its cosmic dust analyzer (CDA) to collect material released from the main rings and to characterize the ring material infall into Saturn. We report the direct in situ detection of material from Saturn's dense rings by the CDA impact mass spectrometer. Most detected grains are a few tens of nanometers in size and dynamically associated with the previously inferred "ring rain." Silicate and water-ice grains were identified, in proportions that vary with latitude. Silicate grains constitute up to 30% of infalling grains, a higher percentage than the bulk silicate content of the rings. |
doi_str_mv | 10.1126/science.aat3185 |
format | article |
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The Cassini spacecraft's traversals between Saturn and its innermost D ring allowed its cosmic dust analyzer (CDA) to collect material released from the main rings and to characterize the ring material infall into Saturn. We report the direct in situ detection of material from Saturn's dense rings by the CDA impact mass spectrometer. Most detected grains are a few tens of nanometers in size and dynamically associated with the previously inferred "ring rain." Silicate and water-ice grains were identified, in proportions that vary with latitude. Silicate grains constitute up to 30% of infalling grains, a higher percentage than the bulk silicate content of the rings.</description><identifier>ISSN: 0036-8075</identifier><identifier>EISSN: 1095-9203</identifier><identifier>DOI: 10.1126/science.aat3185</identifier><identifier>PMID: 30287635</identifier><language>eng</language><publisher>United States: The American Association for the Advancement of Science</publisher><subject>Atmosphere ; Atmospheric entry ; Atmospheric sciences ; Auroras ; Cassini mission ; Charged particles ; Composition ; Cosmic dust ; Deposition ; Dominance ; Dust ; Dust control ; Ejecta ; Ejection ; Emission analysis ; Erosion ; Exploration ; Falling ; Fluctuations ; Grains ; Ice ; Ice formation ; Latitude ; Magnetic fields ; Measuring instruments ; Neutrons ; Orbits ; Radiation ; Radioactive decay ; Rain ; Saturn ; Saturn atmosphere ; Scientific Concepts ; Silica ; Silicates ; Southern Hemisphere ; Spacecraft ; Upper atmosphere ; Water</subject><ispartof>Science (American Association for the Advancement of Science), 2018-10, Vol.362 (6410)</ispartof><rights>Copyright © 2018 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. 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The Cassini spacecraft's traversals between Saturn and its innermost D ring allowed its cosmic dust analyzer (CDA) to collect material released from the main rings and to characterize the ring material infall into Saturn. We report the direct in situ detection of material from Saturn's dense rings by the CDA impact mass spectrometer. Most detected grains are a few tens of nanometers in size and dynamically associated with the previously inferred "ring rain." Silicate and water-ice grains were identified, in proportions that vary with latitude. 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The Cassini spacecraft's traversals between Saturn and its innermost D ring allowed its cosmic dust analyzer (CDA) to collect material released from the main rings and to characterize the ring material infall into Saturn. We report the direct in situ detection of material from Saturn's dense rings by the CDA impact mass spectrometer. Most detected grains are a few tens of nanometers in size and dynamically associated with the previously inferred "ring rain." Silicate and water-ice grains were identified, in proportions that vary with latitude. 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subjects | Atmosphere Atmospheric entry Atmospheric sciences Auroras Cassini mission Charged particles Composition Cosmic dust Deposition Dominance Dust Dust control Ejecta Ejection Emission analysis Erosion Exploration Falling Fluctuations Grains Ice Ice formation Latitude Magnetic fields Measuring instruments Neutrons Orbits Radiation Radioactive decay Rain Saturn Saturn atmosphere Scientific Concepts Silica Silicates Southern Hemisphere Spacecraft Upper atmosphere Water |
title | In situ collection of dust grains falling from Saturn's rings into its atmosphere |
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