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A low accretion efficiency of planetesimals formed at planetary gap edges

Eriksson, Linn E. J. LU ; Ronnet, Thomas LU ; Johansen, Anders LU ; Helled, Ravit ; Valletta, Claudio and Petit, Antoine C. LU orcid (2022) In Astronomy and Astrophysics 661.
Abstract

Observations and models of giant planets indicate that such objects are enriched in heavy elements compared to solar abundances. The prevailing view is that giant planets accreted multiple Earth masses of heavy elements after the end of core formation. Such late solid enrichment is commonly explained by the accretion of planetesimals. Planetesimals are expected to form at the edges of planetary gaps, and here we address the question of whether these planetesimals can be accreted in large enough amounts to explain the inferred high heavy element contents of giant planets. We performed a series of N-body simulations of the dynamics of planetesimals and planets during the planetary growth phase, taking gas drag into account as well... (More)

Observations and models of giant planets indicate that such objects are enriched in heavy elements compared to solar abundances. The prevailing view is that giant planets accreted multiple Earth masses of heavy elements after the end of core formation. Such late solid enrichment is commonly explained by the accretion of planetesimals. Planetesimals are expected to form at the edges of planetary gaps, and here we address the question of whether these planetesimals can be accreted in large enough amounts to explain the inferred high heavy element contents of giant planets. We performed a series of N-body simulations of the dynamics of planetesimals and planets during the planetary growth phase, taking gas drag into account as well as the enhanced collision cross section caused by the extended envelopes. We considered the growth of Jupiter and Saturn via gas accretion after reaching the pebble isolation mass and we included their migration in an evolving disk. We find that the accretion efficiency of planetesimals formed at planetary gap edges is very low: less than 10% of the formed planetesimals are accreted even in the most favorable cases, which in our model corresponds to a few Earth masses. When planetesimals are assumed to form beyond the feeding zone of the planets, extending to a few Hill radii from a planet, accretion becomes negligible. Furthermore, we find that the accretion efficiency increases when the planetary migration distance is increased and that the efficiency does not increase when the planetesimal radii are decreased. Based on these results, we conclude that it is difficult to explain the large heavy element content of giant planets with planetesimal accretion during the gas accretion phase. Alternative processes most likely are required, such as accretion of vapor deposited by drifting pebbles.

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author
; ; ; ; and
organization
publishing date
type
Contribution to journal
publication status
published
subject
keywords
Planet-disk interactions, Planets and satellites: formation, Protoplanetary disks
in
Astronomy and Astrophysics
volume
661
article number
A73
pages
13 pages
publisher
EDP Sciences
external identifiers
  • scopus:85130368374
ISSN
0004-6361
DOI
10.48550/arXiv.2202.12723
language
English
LU publication?
yes
additional info
Publisher Copyright: ©
id
b1c282cd-5f1d-4a5f-9473-1154da886b35
date added to LUP
2022-07-21 10:09:04
date last changed
2024-04-18 08:28:36
@article{b1c282cd-5f1d-4a5f-9473-1154da886b35,
  abstract     = {{<p>Observations and models of giant planets indicate that such objects are enriched in heavy elements compared to solar abundances. The prevailing view is that giant planets accreted multiple Earth masses of heavy elements after the end of core formation. Such late solid enrichment is commonly explained by the accretion of planetesimals. Planetesimals are expected to form at the edges of planetary gaps, and here we address the question of whether these planetesimals can be accreted in large enough amounts to explain the inferred high heavy element contents of giant planets. We performed a series of <i>N</i>-body simulations of the dynamics of planetesimals and planets during the planetary growth phase, taking gas drag into account as well as the enhanced collision cross section caused by the extended envelopes. We considered the growth of Jupiter and Saturn via gas accretion after reaching the pebble isolation mass and we included their migration in an evolving disk. We find that the accretion efficiency of planetesimals formed at planetary gap edges is very low: less than 10% of the formed planetesimals are accreted even in the most favorable cases, which in our model corresponds to a few Earth masses. When planetesimals are assumed to form beyond the feeding zone of the planets, extending to a few Hill radii from a planet, accretion becomes negligible. Furthermore, we find that the accretion efficiency increases when the planetary migration distance is increased and that the efficiency does not increase when the planetesimal radii are decreased. Based on these results, we conclude that it is difficult to explain the large heavy element content of giant planets with planetesimal accretion during the gas accretion phase. Alternative processes most likely are required, such as accretion of vapor deposited by drifting pebbles.</p>}},
  author       = {{Eriksson, Linn E. J. and Ronnet, Thomas and Johansen, Anders and Helled, Ravit and Valletta, Claudio and Petit, Antoine C.}},
  issn         = {{0004-6361}},
  keywords     = {{Planet-disk interactions; Planets and satellites: formation; Protoplanetary disks}},
  language     = {{eng}},
  month        = {{05}},
  publisher    = {{EDP Sciences}},
  series       = {{Astronomy and Astrophysics}},
  title        = {{A low accretion efficiency of planetesimals formed at planetary gap edges}},
  url          = {{http://dx.doi.org/10.48550/arXiv.2202.12723}},
  doi          = {{10.48550/arXiv.2202.12723}},
  volume       = {{661}},
  year         = {{2022}},
}