Carbon-rich dust in comet 67P/Churyumov-Gerasimenko measured by COSIMA/Rosetta
John Paquette; Klaus Hornung; Nicolas Ligier; Laurent Thirkell; Cécile Engrand; Christelle Briois; Harry Lehto; Robin Isnard; Jochen Kissel; Paola Modica; Martin Hilchenbach; François-Régis Orthous-Daunay; Yves Langevin; Kurt Varmuza; Sihane Merouane; Anaïs Bardyn; Henning Fischer; Jouni Rynö; Johan Silén; Boris Zaprudin; Léna Le Roy; Donia Baklouti; Nicolas Fray; Rita Schulz; Hervé Cottin; Oliver Stenzel
https://urn.fi/URN:NBN:fi-fe2021042821678
Tiivistelmä
Cometary ices are rich in CO2, CO and organic volatile
compounds, but the carbon content of cometary dust was only measured for
the Oort Cloud comet 1P/Halley, during its flyby in 1986. The COmetary
Secondary Ion Mass Analyzer (COSIMA)/Rosetta mass spectrometer
analysed dust particles with sizes ranging from 50 to 1000 μm, collected
over 2 yr, from 67P/Churyumov-Gerasimenko (67P), a Jupiter family
comet. Here, we report 67P dust composition focusing on the elements C
and O. It has a high carbon content (atomic |${\rm{C}}/{\rm{Si}} = 5.5{\rm{\ }}_{ - 1.2}^{ + 1.4}\ \ {\rm{on\ average}}$ |)
close to the solar value and comparable to the 1P/Halley data. From
COSIMA measurements, we conclude that 67P particles are made of nearly
50 per cent organic matter in mass, mixed with mineral phases that are
mostly anhydrous. The whole composition, rich in carbon and non-hydrated
minerals, points to a primitive matter that likely preserved its
initial characteristics since the comet accretion in the outer regions
of the protoplanetary disc.
Kokoelmat
- Rinnakkaistallenteet [19207]