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@ARTICLE{Pfalzner:893878,
author = {Pfalzner, Susanne and Aizpuru Vargas, Luis L. and Bhandare,
Asmita and Veras, Dimitri},
title = {{S}ignificant interstellar object production by close
stellar flybys},
journal = {Astronomy and astrophysics},
volume = {651},
issn = {0004-6361},
address = {Les Ulis},
publisher = {EDP Sciences},
reportid = {FZJ-2021-02890},
pages = {A38 -},
year = {2021},
abstract = {Context. Within just two years, two interstellar objects
(ISOs) – 1I/‘Oumuamua and 2I/Borisov – have been
discovered, the first of their kind. Large quantities of
planetesimals form as a by-product of planet formation.
Therefore, it seems likely that ISOs are former
planetesimals that became somehow unbound from their parent
star. The discoveries raise the question of the dominant ISO
formation process.Aims. Here, we concentrate on
planetesimals released during another star’s close flybys.
Such close flybys happen most frequently during the first 10
Myr of a star’s life. Here, we quantify the amount of
planetesimals released during close stellar flybys, their
ejection velocity and likely composition.Methods. We
numerically study the dependence of the effect of parabolic
flybys on the mass ratio between the perturber and parent
star, the periastron distance, inclination, and angle of
periastron.Results. As expected, close prograde flybys of
high-mass stars produce the most considerable amount of
ISOs. Especially flybys of stars with M > 5 M⊙ on
trajectories closer than 250 AU can lead to more
planetesimals turning into ISOs than remaining bound to the
parent star. Even strongly inclined orbits do not
significantly reduce the ISO production; only retrograde
flybys lead to a significantly lower ISO production. For
perturbers slightly more massive than the parent star, there
is a competition between ISO production and planetesimals
being captured by the perturber. Whenever ISOs are produced,
they leave their parent system typically with velocities in
the range of 0.5–2 km s−1. This ejection velocity is
distinctly different to that of ISOs produced by planet
scattering (~4–8 km s−1) and those shed during the
stellar post-main-sequence phase (~0.1–0.2 km s−1).
Using the typical disc truncation radius in various cluster
environments, we find that clusters like the Orion nebula
cluster are likely to produce the equivalent of 0.85
Earth-masses of ISOs per star. In contrast, compact clusters
like NGC 3603 could produce up to 50 Earth-masses of ISOs
per star. Our solar-system probably produced the equivalent
of 2–3 Earth masses of ISOs, which left our solar system
at a mean ejection velocity of 0.7 km s−1.Conclusions.
Most ISOs produced by flybys should be comet-like, similar
to Borisov and unlike ‘Oumuamua. ISOs originating from
compact long-lived clusters would often show a deficiency in
CO. As soon as a statistically significant sample of ISOs is
discovered, the combined information of their observed
velocities and composition might help in constraining the
dominant production process.},
cin = {JSC},
ddc = {520},
cid = {I:(DE-Juel1)JSC-20090406},
pnm = {5111 - Domain-Specific Simulation $\&$ Data Life Cycle Labs
(SDLs) and Research Groups (POF4-511)},
pid = {G:(DE-HGF)POF4-5111},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000672718400004},
doi = {10.1051/0004-6361/202140587},
url = {https://juser.fz-juelich.de/record/893878},
}