Growing the seeds of pebble accretion through planetesimal accretion
Sebastian Lorek, Anders Johansen

TL;DR
This paper models planetary embryo growth via planetesimal accretion, revealing that in outer disc regions, collisional growth is too slow for giant planet formation, emphasizing the importance of pebble accretion on large bodies.
Contribution
The study introduces a comprehensive model combining collisional growth, fragmentation, and velocity evolution to analyze planetesimal and embryo growth across the disc.
Findings
Inner disc regions allow embryo growth within disc lifetime.
Outer disc regions show minimal growth beyond 5-10 AU.
Long timescales hinder collisional growth in planet formation zones.
Abstract
We explore the growth of planetary embryos by planetesimal accretion up to and beyond the point where pebble accretion becomes efficient at the so-called Hill-transition mass. Both the transition mass and the characteristic mass of planetesimals formed by the streaming instability increase with increasing distance from the star. We developed a model for the growth of a large planetesimal (embryo) embedded in a population of smaller planetesimals formed in a filament by the streaming instability. The model includes in a self-consistent way the collisional mass growth of the embryo, the fragmentation of the planetesimals, the velocity evolution of all involved bodies, as well as the viscous spreading of the filament. We find that the embryo accretes all available material in the filament during the lifetime of the protoplanetary disc only in the inner regions of the disc. In contrast, we…
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Taxonomy
TopicsChemical Thermodynamics and Molecular Structure · Astrophysics and Star Formation Studies · Phase Equilibria and Thermodynamics
