TY - JOUR
T1 - Planet seeding through gas-assisted capture of interstellar objects
AU - Grishin, Evgeni
AU - Perets, Hagai B.
AU - Avni, Yael
N1 - Funding Information:
We thank Barak A. Katzir and Andrei P. Igoshev for stimulating discussions. EG acknowledges support by the Technion Irwin and Joan Jacobs Excellence Fellowship for outstanding graduate students. EG and HBP acknowledge support by Israel Science Foundation I-CORE grant 1829/12 and the Minerva center for life under extreme planetary conditions.
Publisher Copyright:
© 2019 The Author(s) Published by Oxford University Press on behalf of the Royal Astronomical Society.
Copyright:
Copyright 2021 Elsevier B.V., All rights reserved.
PY - 2019/8/11
Y1 - 2019/8/11
N2 - Planet formation begins with collisional growth of small planetesimals accumulating into larger ones. Such growth occurs while planetesimals are embedded in a gaseous protoplanetary disc. However, small planetesimals experience collisions and gas drag that lead to their destruction on short time-scales, not allowing, or requiring fine-tuned conditions for the efficient growth of ∼metre-sized objects. Here we show that ∼104 interstellar objects such as the recently detected 1I/2017-U1 ('Oumuamua) could have been captured, and become part of the young Solar system, together with up to hundreds of ∼km-sized ones. The capture rates are robust even for conservative assumptions on the protoplanetary disc structure, local stellar environment, and planetesimal interstellar medium density. 'Seeding' of such planetesimals then catalyses further planetary growth into planetary embryos, and potentially alleviates the main challenges with the metre-sized growth barrier. The capture model is in synergy with the current leading planet formation theories, providing the missing link to the first planetesimals. Moreover, planetesimal capture provides a far more efficient route for lithopanspermia than previously thought.
AB - Planet formation begins with collisional growth of small planetesimals accumulating into larger ones. Such growth occurs while planetesimals are embedded in a gaseous protoplanetary disc. However, small planetesimals experience collisions and gas drag that lead to their destruction on short time-scales, not allowing, or requiring fine-tuned conditions for the efficient growth of ∼metre-sized objects. Here we show that ∼104 interstellar objects such as the recently detected 1I/2017-U1 ('Oumuamua) could have been captured, and become part of the young Solar system, together with up to hundreds of ∼km-sized ones. The capture rates are robust even for conservative assumptions on the protoplanetary disc structure, local stellar environment, and planetesimal interstellar medium density. 'Seeding' of such planetesimals then catalyses further planetary growth into planetary embryos, and potentially alleviates the main challenges with the metre-sized growth barrier. The capture model is in synergy with the current leading planet formation theories, providing the missing link to the first planetesimals. Moreover, planetesimal capture provides a far more efficient route for lithopanspermia than previously thought.
KW - astrobiology
KW - comets: general
KW - minor planets, asteroids: general
KW - minor planets, asteroids: individual: 1I/2017 U1 ('Oumuamua)
KW - planets and satellites: formation
UR - https://www.scopus.com/pages/publications/85072331597
U2 - 10.1093/mnras/stz1505
DO - 10.1093/mnras/stz1505
M3 - Article
AN - SCOPUS:85072331597
SN - 0035-8711
VL - 487
SP - 3324
EP - 3332
JO - Monthly Notices of the Royal Astronomical Society
JF - Monthly Notices of the Royal Astronomical Society
IS - 3
ER -