Literature DB >> 25791084

Molecular nitrogen in comet 67P/Churyumov-Gerasimenko indicates a low formation temperature.

M Rubin1, K Altwegg2, H Balsiger3, A Bar-Nun4, J-J Berthelier5, A Bieler6, P Bochsler3, C Briois7, U Calmonte3, M Combi8, J De Keyser9, F Dhooghe9, P Eberhardt3, B Fiethe10, S A Fuselier11, S Gasc3, T I Gombosi8, K C Hansen8, M Hässig12, A Jäckel3, E Kopp3, A Korth13, L Le Roy14, U Mall13, B Marty15, O Mousis16, T Owen17, H Rème18, T Sémon3, C-Y Tzou3, J H Waite11, P Wurz3.   

Abstract

Molecular nitrogen (N2) is thought to have been the most abundant form of nitrogen in the protosolar nebula. It is the main N-bearing molecule in the atmospheres of Pluto and Triton and probably the main nitrogen reservoir from which the giant planets formed. Yet in comets, often considered the most primitive bodies in the solar system, N2 has not been detected. Here we report the direct in situ measurement of N2 in the Jupiter family comet 67P/Churyumov-Gerasimenko, made by the Rosetta Orbiter Spectrometer for Ion and Neutral Analysis mass spectrometer aboard the Rosetta spacecraft. A N2/CO ratio of (5.70 ± 0.66) × 10(-3) (2σ standard deviation of the sampled mean) corresponds to depletion by a factor of ~25.4 ± 8.9 as compared to the protosolar value. This depletion suggests that cometary grains formed at low-temperature conditions below ~30 kelvin.
Copyright © 2015, American Association for the Advancement of Science.

Entities:  

Year:  2015        PMID: 25791084     DOI: 10.1126/science.aaa6100

Source DB:  PubMed          Journal:  Science        ISSN: 0036-8075            Impact factor:   47.728


  14 in total

1.  Abundant molecular oxygen in the coma of comet 67P/Churyumov-Gerasimenko.

Authors:  A Bieler; K Altwegg; H Balsiger; A Bar-Nun; J-J Berthelier; P Bochsler; C Briois; U Calmonte; M Combi; J De Keyser; E F van Dishoeck; B Fiethe; S A Fuselier; S Gasc; T I Gombosi; K C Hansen; M Hässig; A Jäckel; E Kopp; A Korth; L Le Roy; U Mall; R Maggiolo; B Marty; O Mousis; T Owen; H Rème; M Rubin; T Sémon; C-Y Tzou; J H Waite; C Walsh; P Wurz
Journal:  Nature       Date:  2015-10-29       Impact factor: 49.962

2.  PLANET TOPERS: Planets, Tracing the Transfer, Origin, Preservation, and Evolution of their ReservoirS.

Authors:  V Dehant; D Asael; R M Baland; B K Baludikay; J Beghin; J Belza; M Beuthe; D Breuer; S Chernonozhkin; Ph Claeys; Y Cornet; L Cornet; A Coyette; V Debaille; C Delvigne; M H Deproost; N De WInter; C Duchemin; F El Atrassi; C François; J De Keyser; C Gillmann; E Gloesener; S Goderis; Y Hidaka; D Höning; M Huber; G Hublet; E J Javaux; Ö Karatekin; J Kodolanyi; L Lobo Revilla; L Maes; R Maggiolo; N Mattielli; M Maurice; S McKibbin; A Morschhauser; W Neumann; L Noack; L B S Pham; L Pittarello; A C Plesa; A Rivoldini; S Robert; P Rosenblatt; T Spohn; J -Y Storme; N Tosi; A Trinh; M Valdes; A C Vandaele; F Vanhaecke; T Van Hoolst; N Van Roosbroek; V Wilquet; M Yseboodt
Journal:  Orig Life Evol Biosph       Date:  2016-06-23       Impact factor: 1.950

3.  Implementation of Precursor and Neutral Loss Scans on a Miniature Ion Trap Mass Spectrometer and Performance Comparison to a Benchtop Linear Ion Trap.

Authors:  Dalton T Snyder; Lucas J Szalwinski; Ryan Hilger; R Graham Cooks
Journal:  J Am Soc Mass Spectrom       Date:  2018-03-13       Impact factor: 3.109

4.  Water Reservoirs in Small Planetary Bodies: Meteorites, Asteroids, and Comets.

Authors:  Conel M O'D Alexander; Kevin D McKeegan; Kathrin Altwegg
Journal:  Space Sci Rev       Date:  2018-01-23       Impact factor: 8.017

5.  Simulations of ice chemistry in cometary nuclei.

Authors:  Robin T Garrod
Journal:  Astrophys J       Date:  2019-10-14       Impact factor: 5.874

6.  Anoxic and Oxic Oxidation of Rocks Containing Fe(II)Mg-Silicates and Fe(II)-Monosulfides as Source of Fe(III)-Minerals and Hydrogen. Geobiotropy.

Authors:  Marie-Paule Bassez
Journal:  Orig Life Evol Biosph       Date:  2017-03-31       Impact factor: 1.950

7.  The Surface Distributions of the Production of the Major Volatile Species, H2O, CO2, CO and O2, from the Nucleus of Comet 67P/Churyumov-Gerasimenko throughout the Rosetta Mission as Measured by the ROSINA Double Focusing Mass Spectrometer.

Authors:  Michael Combi; Yinsi Shou; Nicolas Fougere; Valeriy Tenishev; Kathrin Altwegg; Martin Rubin; Dominique Bockelée-Morvan; Fabrizio Capaccioni; Yu-Chi Cheng; Uwe Fink; Tamas Gombosi; Kenneth C Hansen; Zhenguang Huang; David Marshall; Gabor Toth
Journal:  Icarus       Date:  2020-01       Impact factor: 3.508

Review 8.  The Rosetta mission orbiter science overview: the comet phase.

Authors:  M G G T Taylor; N Altobelli; B J Buratti; M Choukroun
Journal:  Philos Trans A Math Phys Eng Sci       Date:  2017-07-13       Impact factor: 4.226

9.  Detection of argon in the coma of comet 67P/Churyumov-Gerasimenko.

Authors:  Hans Balsiger; Kathrin Altwegg; Akiva Bar-Nun; Jean-Jacques Berthelier; Andre Bieler; Peter Bochsler; Christelle Briois; Ursina Calmonte; Michael Combi; Johan De Keyser; Peter Eberhardt; Björn Fiethe; Stephen A Fuselier; Sébastien Gasc; Tamas I Gombosi; Kenneth C Hansen; Myrtha Hässig; Annette Jäckel; Ernest Kopp; Axel Korth; Lena Le Roy; Urs Mall; Bernard Marty; Olivier Mousis; Tobias Owen; Henri Rème; Martin Rubin; Thierry Sémon; Chia-Yu Tzou; J Hunter Waite; Peter Wurz
Journal:  Sci Adv       Date:  2015-09-25       Impact factor: 14.136

10.  Photochemistry of forbidden oxygen lines in the inner coma of 67P/Churyumov-Gerasimenko.

Authors:  G Cessateur; J De Keyser; R Maggiolo; A Gibbons; G Gronoff; H Gunell; F Dhooghe; J Loreau; N Vaeck; K Altwegg; A Bieler; C Briois; U Calmonte; M R Combi; B Fiethe; S A Fuselier; T I Gombosi; M Hässig; L Le Roy; E Neefs; M Rubin; T Sémon
Journal:  J Geophys Res Space Phys       Date:  2016-01-28       Impact factor: 2.811

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