1I/'Oumuamua as an N2 ice fragment of an exo-pluto surface. II. Generation of N2 ice fragments and the origin of 'Oumuamua
Steven J. Desch, Alan P. Jackson

TL;DR
This paper proposes that 'Oumuamua is an N2 ice fragment ejected from a Pluto-like exoplanet, supported by models of impact fragmentation on Kuiper belt objects and their ejection into interstellar space.
Contribution
It demonstrates that impact-generated N2 ice fragments from Kuiper belt objects can explain 'Oumuamua's properties and their ejection is likely common in other stellar systems.
Findings
Impact on Kuiper belt objects produces ~10^14 fragments.
Fragments can survive cosmic ray erosion over billions of years.
'Oumuamua likely ejected 0.4-0.5 Gyr ago from a young stellar system.
Abstract
The origin of the interstellar object 1I/'Oumuamua, has defied explanation. In a companion paper (Jackson & Desch, 2021), we show that a body of N2 ice with axes 45 m x 44 m x 7.5 m at the time of observation would be consistent with its albedo, non-gravitational acceleration, and lack of observed CO or CO2 or dust. Here we demonstrate that impacts on the surfaces of Pluto-like Kuiper belt objects (KBOs) would have generated and ejected ~10^14 collisional fragments--roughly half of them H2O ice fragments and half of them N2 ice fragments--due to the dynamical instability that depleted the primordial Kuiper belt. We show consistency between these numbers and the frequency with which we would observe interstellar objects like 1I/'Oumuamua, and more comet-like objects like 2I/Borisov, if other stellar systems eject such objects with efficiency like that of the Sun; we infer that…
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