Exploring the conditions for forming cold gas giants through planetesimal accretion
Anders Johansen (Lund Observatory), Bertram Bitsch (Max Planck, Institute for Astronomy)

TL;DR
This study models the formation of cold gas giants via planetesimal accretion, revealing that a massive planetesimal reservoir alone is insufficient, and specific conditions like small planetesimals and weak turbulence are necessary.
Contribution
It demonstrates that forming cold gas giants through planetesimal accretion requires conditions that violate typical solar system constraints, highlighting the need for specific small planetesimals and weak turbulence.
Findings
Massive planetesimal reservoirs alone cannot form cold gas giants.
Weak turbulence and small planetesimals are necessary for cold gas giant formation.
Standard constraints are incompatible with the formation of cold gas giants via planetesimal accretion.
Abstract
The formation of cold gas giants similar to Jupiter and Saturn in orbit and mass is a great challenge for planetesimal-driven core accretion models because the core growth rates far from the star are low. Here we model the growth and migration of single protoplanets that accrete planetesimals and gas. We integrated the core growth rate using fits in the literature to -body simulations, which provide the efficiency of accreting the planetesimals that a protoplanet migrates through. We take into account three constraints from the solar system and from protoplanetary discs: (1) the masses of the terrestrial planets and the comet reservoirs in Neptune's scattered disc and the Oort cloud are consistent with a primordial planetesimal population of a few Earth masses per AU, (2) evidence from the asteroid belt and the Kuiper belt indicates that the characteristic planetesimal diameter is…
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