In-Situ Formation of the Cold Classical Kuiper Belt
Rixin Li, Eugene Chiang

TL;DR
This paper demonstrates through 3D simulations that the Cold Classical Kuiper Belt formed in situ from a small fraction of the solar nebula's solids, explaining its mass, size, and binary properties.
Contribution
It provides a novel in-situ formation model for the CCKB using realistic mass estimates and explains binary formation, contrasting with previous models that assumed excessive mass.
Findings
CCKB formed from about 1% of the original nebular solids.
Simulations reproduce characteristic sizes and binary properties of CCKB objects.
Other formation scenarios like pressure bump trapping are less consistent with observations.
Abstract
Cold Classical Kuiper belt objects (CCKBOs) are considered first-generation planetesimals that formed 42-47 au from the Sun and remained untouched since. Formation is thought to proceed by clumping of dust particles in protoplanetary disk gas by the streaming instability, followed by gravitational collapse. Previous calculations along these lines are inconsistent with the CCKB's supposedly pristine nature, because they assume orders of magnitude more solid mass than is actually present in the CCKB (a few thousandths of an Earth mass) and do not explain how to expel the >99% extra mass. Here we show from 3D numerical simulations of dust and gas that the total mass in CCKBOs, their characteristic sizes of ~100 km, and the relative proportion of prograde to retrograde binaries can all be reproduced at the tail end of the solar nebula's life, when it contained just 2-5% of its original…
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