A1 Refereed original research article in a scientific journal
Optical properties of cometary particles collected by the COSIMA mass spectrometer on-board Rosetta during the rendezvous phase around comet 67P/Churyumov–Gerasimenko
Authors: Y. Langevin, M. Hilchenbach, M. Vincendon, S. Merouane, K. Hornung, N. Ligier, C. Engrand, R. Schulz, J. Kissel, J. Rynö; the COSIMA team
Publication year: 2017
Journal: Monthly Notices of the Royal Astronomical Society
Volume: 469
Issue: Supplement: 2
First page : S535
Last page: S549
Number of pages: 15
ISSN: 0035-8711
eISSN: 1365-2966
DOI: https://doi.org/10.1093/mnras/stx2070(external)
Web address : https://academic.oup.com/mnras/article/469/Suppl_2/S535/4082737(external)
Self-archived copy’s web address: https://research.utu.fi/converis/portal/detail/Publication/38998064(external)
40 000 collected cometary particles have been identified on the 21 targets exposed by the COSIMA experiment on-board Rosetta
to the environment of comet 67P/Churyumov–Gerasimenko from 2014 August
to 2016 September. The images of the targets where obtained by the
COSIMA microscope (Cosiscope, 13.95 μm pixel−1) with near
grazing incidence, which is optimal for the primary objective (detection
of collected particles) but very challenging for photometry. However,
more than 300 of the collected particles are larger than 100 μm which
makes it possible to derive constraints on the optical properties from
the distribution of light levels within the particles. Two types of
particles collected by COSIMA (compact particles and cluster particles)
have been identified in Langevin et al. The best estimate reflectance
factors of compact particles range from 10 per cent to 23 per cent. For
cluster particles (>90 per cent of large collected particles), the
comparison of the signal profiles with illumination from two opposite
directions shows that there is scattering within the particles, with a
mean free path in the 20–25 μm range, which requires high porosity. The
best estimate reflectance factors of cluster particles range from
3 per cent to 22 per cent. This range of reflectance factors overlaps
with that obtained from observations of the cometary nucleus at
macroscopic scales by OSIRIS and it is consistent with that measured for
interplanetary dust particles collected in the stratosphere of the
Earth.
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