Challenges in Forming the Solar System's Giant Planet Cores via Pebble Accretion
K. A. Kretke, H. F. Levison

TL;DR
This paper explores the challenges of forming giant planet cores via pebble accretion in a multi-planet system, revealing that it often results in oligarchic growth inconsistent with our solar system.
Contribution
The study incorporates pebble accretion physics into a global simulation code to analyze its effects in a multi-planet environment, highlighting limitations of current models.
Findings
Pebble accretion leads to oligarchic growth of similar-sized planets.
Hundreds of Mars- and Earth-mass objects form between 4 and 10 AU.
Common mechanisms like evaporation fronts do not prevent oligarchic growth.
Abstract
Though ~10 Earth mass rocky/icy cores are commonly held as a prerequisite for the formation of gas giants, theoretical models still struggle to explain how these embryos can form within the lifetimes of gaseous circumstellar disks. In recent years, aerodynamic-aided accretion of "pebbles," objects ranging from centimeters to meters in size, has been suggested as a potential solution to this long-standing problem. While pebble accretion has been demonstrated to be extremely effective in local simulations that look at the detailed behavior of these pebbles in the vicinity of a single planetary embryo, to date there have been no global simulations demonstrating the effectiveness of pebble accretion in a more complicated, multi-planet environment. Therefore, we have incorporated the aerodynamic-aided accretion physics into LIPAD, a Lagrangian code that can follow the collisional /…
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