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Nitrogen-to-carbon atomic ratio measured by COSIMA in the particles of comet 67P/Churyumov–Gerasimenko

Cécile Engrand; Robin Isnard; Jochen Kissel; Yves Langevin; Johan Silén; Boris Zaprudin; Sandra Siljeström Oliver Stenzel; Léna Le Roy; Christelle Briois; Laurent Thirkell; Jouni Rynö; Klaus Hornung; Anaïs Bardyn; John Paquette; Paola Modica; Kurt Varmuza; Donia Baklouti; Nicolas Fray; Harry Lehto; Rita Schulz; Eva Maria Mellado; Henning Fischer; Hervé Cottin; Sihane Merouane; Martin Hilchenbach; François-Régis Orthous-Daunay

Nitrogen-to-carbon atomic ratio measured by COSIMA in the particles of comet 67P/Churyumov–Gerasimenko

Cécile Engrand
Robin Isnard
Jochen Kissel
Yves Langevin
Johan Silén
Boris Zaprudin
Sandra Siljeström Oliver Stenzel
Léna Le Roy
Christelle Briois
Laurent Thirkell
Jouni Rynö
Klaus Hornung
Anaïs Bardyn
John Paquette
Paola Modica
Kurt Varmuza
Donia Baklouti
Nicolas Fray
Harry Lehto
Rita Schulz
Eva Maria Mellado
Henning Fischer
Hervé Cottin
Sihane Merouane
Martin Hilchenbach
François-Régis Orthous-Daunay
Katso/Avaa
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Oxford University Press
doi:10.1093/mnras/stx2002
URI
https://academic.oup.com/mnras/article/469/Suppl_2/S506/4067798
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Julkaisun pysyvä osoite on:
https://urn.fi/URN:NBN:fi-fe2021042718454
Tiivistelmä

The COmetary Secondary Ion Mass Analyzer (COSIMA) on board the Rosetta mission has analysed numerous cometary dust particles collected at very low velocities (a few m s−1)
in the environment of comet 67P/Churyumov–Gerasimenko (hereafter 67P).
In these particles, carbon and nitrogen are expected mainly to be part
of the organic matter. We have measured the nitrogen-to-carbon (N/C)
atomic ratio of 27 cometary particles. It ranges from 0.018 to 0.06 with
an averaged value of 0.035 ± 0.011. This is compatible with the
measurements of the particles of comet 1P/Halley and is in the lower
range of the values measured in comet 81P/Wild 2 particles brought back
to Earth by the Stardust mission. Moreover, the averaged value
found in 67P particles is also similar to the one found in the insoluble
organic matter extracted from CM, CI and CR carbonaceous chondrites and
to the bulk values measured in most interplanetary dust particles and
micrometeorites. The close agreement of the N/C atomic ratio in all
these objects indicates that their organic matters share some
similarities and could have a similar chemical origin. Furthermore,
compared to the abundances of all the detected elements in the particles
of 67P and to the elemental solar abundances, the nitrogen is depleted
in the particles and the nucleus of 67P as was previously inferred also
for comet 1P/Halley. This nitrogen depletion could constrain the
formation scenarios of cometary nuclei.

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