Carbon Chain Anions and the Growth of Complex Organic Molecules in Titan's Ionosphere
Cassini discovered a plethora of neutral and ionized molecules in Titan's ionosphere including, surprisingly, anions and negatively charged molecules extending up to 13,800 u q−1. In this Letter, we forward model the Cassini electron spectrometer response function to this unexpected ionospheric...
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creator | Desai, R. T. Coates, A. J. Wellbrock, A. Vuitton, V. Crary, F. J. González-Caniulef, D. Shebanits, O. Jones, G. H. Lewis, G. R. Waite, J. H. Cordiner, M. Taylor, S. A. Kataria, D. O. Wahlund, J.-E. Edberg, N. J. T. Sittler, E. C. |
description | Cassini discovered a plethora of neutral and ionized molecules in Titan's ionosphere including, surprisingly, anions and negatively charged molecules extending up to 13,800 u q−1. In this Letter, we forward model the Cassini electron spectrometer response function to this unexpected ionospheric component to achieve an increased mass resolving capability for negatively charged species observed at Titan altitudes of 950-1300 km. We report on detections consistently centered between 25.8 and 26.0 u q−1 and between 49.0-50.1 u q−1 which are identified as belonging to the carbon chain anions, CN−/C3N− and/or C2H−/C4H−, in agreement with chemical model predictions. At higher ionospheric altitudes, detections at 73-74 u q−1 could be attributed to the further carbon chain anions C5N−/C6H− but at lower altitudes and during further encounters extend over a higher mass/charge range. This, as well as further intermediary anions detected at >100 u, provide the first evidence for efficient anion chemistry in space involving structures other than linear chains. Furthermore, at altitudes below |
doi_str_mv | 10.3847/2041-8213/aa7851 |
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T. ; Coates, A. J. ; Wellbrock, A. ; Vuitton, V. ; Crary, F. J. ; González-Caniulef, D. ; Shebanits, O. ; Jones, G. H. ; Lewis, G. R. ; Waite, J. H. ; Cordiner, M. ; Taylor, S. A. ; Kataria, D. O. ; Wahlund, J.-E. ; Edberg, N. J. T. ; Sittler, E. C.</creator><creatorcontrib>Desai, R. T. ; Coates, A. J. ; Wellbrock, A. ; Vuitton, V. ; Crary, F. J. ; González-Caniulef, D. ; Shebanits, O. ; Jones, G. H. ; Lewis, G. R. ; Waite, J. H. ; Cordiner, M. ; Taylor, S. A. ; Kataria, D. O. ; Wahlund, J.-E. ; Edberg, N. J. T. ; Sittler, E. C.</creatorcontrib><description>Cassini discovered a plethora of neutral and ionized molecules in Titan's ionosphere including, surprisingly, anions and negatively charged molecules extending up to 13,800 u q−1. In this Letter, we forward model the Cassini electron spectrometer response function to this unexpected ionospheric component to achieve an increased mass resolving capability for negatively charged species observed at Titan altitudes of 950-1300 km. We report on detections consistently centered between 25.8 and 26.0 u q−1 and between 49.0-50.1 u q−1 which are identified as belonging to the carbon chain anions, CN−/C3N− and/or C2H−/C4H−, in agreement with chemical model predictions. At higher ionospheric altitudes, detections at 73-74 u q−1 could be attributed to the further carbon chain anions C5N−/C6H− but at lower altitudes and during further encounters extend over a higher mass/charge range. This, as well as further intermediary anions detected at >100 u, provide the first evidence for efficient anion chemistry in space involving structures other than linear chains. Furthermore, at altitudes below <1100 km, the low-mass anions (<150 u q−1) were found to deplete at a rate proportional to the growth of the larger molecules, a correlation that indicates the anions are tightly coupled to the growth process. This study adds Titan to an increasing list of astrophysical environments where chain anions have been observed and shows that anion chemistry plays a role in the formation of complex organics within a planetary atmosphere as well as in the interstellar medium.</description><identifier>ISSN: 2041-8205</identifier><identifier>ISSN: 2041-8213</identifier><identifier>EISSN: 2041-8213</identifier><identifier>DOI: 10.3847/2041-8213/aa7851</identifier><language>eng</language><publisher>Austin: The American Astronomical Society</publisher><subject>ALTITUDE ; Anions ; astrobiology ; astrochemistry ; ASTROPHYSICS ; ASTROPHYSICS, COSMOLOGY AND ASTRONOMY ; CARBON ; CARBON NITRIDES ; Cassini mission ; CORRELATIONS ; DETECTION ; ELECTRON SPECTROMETERS ; FORECASTING ; Interstellar matter ; Interstellar medium ; IONOSPHERE ; Ionospheric models ; Ions ; ISM: molecules ; MASS ; Molecular chains ; MOLECULES ; Organic chemistry ; Planet formation ; PLANETARY ATMOSPHERES ; PLANETS ; planets and satellites: atmospheres ; planets and satellites: individual (Titan) ; RESPONSE FUNCTIONS ; SATELLITE ATMOSPHERES ; SATELLITES ; Sciences of the Universe ; SPACE ; Titan</subject><ispartof>Astrophysical journal. Letters, 2017-08, Vol.844 (2), p.L18</ispartof><rights>2017. The American Astronomical Society. All rights reserved.</rights><rights>Copyright IOP Publishing Aug 01, 2017</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c516t-ffcac2679201f60951fc876bf0855d3a936b53c7f0934a85f4c1eb3d24106ee93</citedby><cites>FETCH-LOGICAL-c516t-ffcac2679201f60951fc876bf0855d3a936b53c7f0934a85f4c1eb3d24106ee93</cites><orcidid>0000-0001-9621-211X ; 0000-0001-5848-0180 ; 0000-0002-1261-7580 ; 0000-0001-5213-7947 ; 0000-0002-2015-4053 ; 0000-0001-7273-1898 ; 0000-0002-2107-5859 ; 0000-0002-1978-1025 ; 0000-0002-6185-3125 ; 0000-0001-8233-2436</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://iopscience.iop.org/article/10.3847/2041-8213/aa7851/pdf$$EPDF$$P50$$Giop$$Hfree_for_read</linktopdf><link.rule.ids>230,314,550,776,780,881,27901,27902,38845,38867,53815,53842</link.rule.ids><backlink>$$Uhttps://insu.hal.science/insu-03692489$$DView record in HAL$$Hfree_for_read</backlink><backlink>$$Uhttps://www.osti.gov/biblio/22654427$$D View this record in Osti.gov$$Hfree_for_read</backlink><backlink>$$Uhttps://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-332933$$DView record from Swedish Publication Index$$Hfree_for_read</backlink></links><search><creatorcontrib>Desai, R. T.</creatorcontrib><creatorcontrib>Coates, A. J.</creatorcontrib><creatorcontrib>Wellbrock, A.</creatorcontrib><creatorcontrib>Vuitton, V.</creatorcontrib><creatorcontrib>Crary, F. J.</creatorcontrib><creatorcontrib>González-Caniulef, D.</creatorcontrib><creatorcontrib>Shebanits, O.</creatorcontrib><creatorcontrib>Jones, G. H.</creatorcontrib><creatorcontrib>Lewis, G. R.</creatorcontrib><creatorcontrib>Waite, J. H.</creatorcontrib><creatorcontrib>Cordiner, M.</creatorcontrib><creatorcontrib>Taylor, S. A.</creatorcontrib><creatorcontrib>Kataria, D. O.</creatorcontrib><creatorcontrib>Wahlund, J.-E.</creatorcontrib><creatorcontrib>Edberg, N. J. T.</creatorcontrib><creatorcontrib>Sittler, E. C.</creatorcontrib><title>Carbon Chain Anions and the Growth of Complex Organic Molecules in Titan's Ionosphere</title><title>Astrophysical journal. Letters</title><addtitle>APJL</addtitle><addtitle>Astrophys. J. Lett</addtitle><description>Cassini discovered a plethora of neutral and ionized molecules in Titan's ionosphere including, surprisingly, anions and negatively charged molecules extending up to 13,800 u q−1. In this Letter, we forward model the Cassini electron spectrometer response function to this unexpected ionospheric component to achieve an increased mass resolving capability for negatively charged species observed at Titan altitudes of 950-1300 km. We report on detections consistently centered between 25.8 and 26.0 u q−1 and between 49.0-50.1 u q−1 which are identified as belonging to the carbon chain anions, CN−/C3N− and/or C2H−/C4H−, in agreement with chemical model predictions. At higher ionospheric altitudes, detections at 73-74 u q−1 could be attributed to the further carbon chain anions C5N−/C6H− but at lower altitudes and during further encounters extend over a higher mass/charge range. This, as well as further intermediary anions detected at >100 u, provide the first evidence for efficient anion chemistry in space involving structures other than linear chains. Furthermore, at altitudes below <1100 km, the low-mass anions (<150 u q−1) were found to deplete at a rate proportional to the growth of the larger molecules, a correlation that indicates the anions are tightly coupled to the growth process. This study adds Titan to an increasing list of astrophysical environments where chain anions have been observed and shows that anion chemistry plays a role in the formation of complex organics within a planetary atmosphere as well as in the interstellar medium.</description><subject>ALTITUDE</subject><subject>Anions</subject><subject>astrobiology</subject><subject>astrochemistry</subject><subject>ASTROPHYSICS</subject><subject>ASTROPHYSICS, COSMOLOGY AND ASTRONOMY</subject><subject>CARBON</subject><subject>CARBON NITRIDES</subject><subject>Cassini mission</subject><subject>CORRELATIONS</subject><subject>DETECTION</subject><subject>ELECTRON SPECTROMETERS</subject><subject>FORECASTING</subject><subject>Interstellar matter</subject><subject>Interstellar medium</subject><subject>IONOSPHERE</subject><subject>Ionospheric models</subject><subject>Ions</subject><subject>ISM: molecules</subject><subject>MASS</subject><subject>Molecular chains</subject><subject>MOLECULES</subject><subject>Organic chemistry</subject><subject>Planet formation</subject><subject>PLANETARY ATMOSPHERES</subject><subject>PLANETS</subject><subject>planets and satellites: atmospheres</subject><subject>planets and satellites: individual (Titan)</subject><subject>RESPONSE FUNCTIONS</subject><subject>SATELLITE ATMOSPHERES</subject><subject>SATELLITES</subject><subject>Sciences of the Universe</subject><subject>SPACE</subject><subject>Titan</subject><issn>2041-8205</issn><issn>2041-8213</issn><issn>2041-8213</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>O3W</sourceid><sourceid>D8T</sourceid><recordid>eNp1kc9LwzAYhosoqNO7x4AHQZzmR5M2x1F1Eya7bF5DmiU2UpOatE7_ezsqGx48fR8fz_fAy5skFwjekjzN7jBM0TjHiNxJmeUUHSQnu9Phbof0ODmN8Q1CDBnKT5JVIUPpHSgqaR2YOOtdBNKtQVtpMA1-01bAG1D496bWX2ARXqWzCjz7Wquu1hH0X0vbSncVwZN3PjaVDvosOTKyjvr8d46S1ePDspiN54vpUzGZjxVFrB0bo6TCLOMYIsMgp8ioPGOlgTmlayI5YSUlKjOQk1Tm1KQK6ZKscYog05qTUXIzeONGN10pmmDfZfgWXlpxb18mwodX0XWCEMwJ6fHLAfextSIq22pVKe-cVq3AmNE0xVlPXQ9UJes_xtlkLqyLnYCEcZzm_BPtlU3wH52OrXjzXXB9aIEJo4wgTmhPwYFSwccYtNl5ERTb-sS2H7HtSgz17aNZ3-yd_-I_gByYEg</recordid><startdate>20170801</startdate><enddate>20170801</enddate><creator>Desai, R. 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T. ; Coates, A. J. ; Wellbrock, A. ; Vuitton, V. ; Crary, F. J. ; González-Caniulef, D. ; Shebanits, O. ; Jones, G. H. ; Lewis, G. R. ; Waite, J. H. ; Cordiner, M. ; Taylor, S. A. ; Kataria, D. O. ; Wahlund, J.-E. ; Edberg, N. J. T. ; Sittler, E. 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Lett</addtitle><date>2017-08-01</date><risdate>2017</risdate><volume>844</volume><issue>2</issue><spage>L18</spage><pages>L18-</pages><issn>2041-8205</issn><issn>2041-8213</issn><eissn>2041-8213</eissn><abstract>Cassini discovered a plethora of neutral and ionized molecules in Titan's ionosphere including, surprisingly, anions and negatively charged molecules extending up to 13,800 u q−1. In this Letter, we forward model the Cassini electron spectrometer response function to this unexpected ionospheric component to achieve an increased mass resolving capability for negatively charged species observed at Titan altitudes of 950-1300 km. We report on detections consistently centered between 25.8 and 26.0 u q−1 and between 49.0-50.1 u q−1 which are identified as belonging to the carbon chain anions, CN−/C3N− and/or C2H−/C4H−, in agreement with chemical model predictions. At higher ionospheric altitudes, detections at 73-74 u q−1 could be attributed to the further carbon chain anions C5N−/C6H− but at lower altitudes and during further encounters extend over a higher mass/charge range. This, as well as further intermediary anions detected at >100 u, provide the first evidence for efficient anion chemistry in space involving structures other than linear chains. Furthermore, at altitudes below <1100 km, the low-mass anions (<150 u q−1) were found to deplete at a rate proportional to the growth of the larger molecules, a correlation that indicates the anions are tightly coupled to the growth process. 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subjects | ALTITUDE Anions astrobiology astrochemistry ASTROPHYSICS ASTROPHYSICS, COSMOLOGY AND ASTRONOMY CARBON CARBON NITRIDES Cassini mission CORRELATIONS DETECTION ELECTRON SPECTROMETERS FORECASTING Interstellar matter Interstellar medium IONOSPHERE Ionospheric models Ions ISM: molecules MASS Molecular chains MOLECULES Organic chemistry Planet formation PLANETARY ATMOSPHERES PLANETS planets and satellites: atmospheres planets and satellites: individual (Titan) RESPONSE FUNCTIONS SATELLITE ATMOSPHERES SATELLITES Sciences of the Universe SPACE Titan |
title | Carbon Chain Anions and the Growth of Complex Organic Molecules in Titan's Ionosphere |
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