The Formation of Uranus and Neptune in Solid-Rich Feeding Zones: Connecting Chemistry and Dynamics
Sarah E. Dodson-Robinson (1), Peter Bodenheimer (2) ((1) University of, Texas, (2) UCO/Lick Observatory)

TL;DR
This paper presents new simulations showing that Uranus and Neptune could form more quickly and with subcritical cores in solid-rich zones, resolving key issues in the core accretion theory of ice giant formation.
Contribution
The study demonstrates that migration in solid-rich disks leads to faster formation of ice giants with realistic core masses, aligning with observed compositions and challenging previous formation models.
Findings
Uranus and Neptune form in 3.8-6 Myr, faster than previous models.
Core masses remain subcritical, avoiding sudden gas accretion cutoff.
Simulations match observed ice giant compositions and methane ice content.
Abstract
The core accretion theory of planet formation has at least two fundamental problems explaining the origins of Uranus and Neptune: (1) dynamical times in the trans-Saturnian solar nebula are so long that core growth can take > 15 Myr, and (2) the onset of runaway gas accretion that begins when cores reach 10 Earth masses necessitates a sudden gas accretion cutoff just as the ice giant cores reach critical mass. Both problems may be resolved by allowing the ice giants to migrate outward after their formation in solid-rich feeding zones with planetesimal surface densities well above the minimum-mass solar nebula. We present new simulations of the formation of Uranus and Neptune in the solid-rich disk of Dodson-Robinson et al. (2009) using the initial semimajor axis distribution of the Nice model (Gomes et al. 2005; Morbidelli et al. 2005; Tsiganis et al. 2005), with one ice giant forming…
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