1. Solid accretion onto planetary cores in radiative disks
- Author
-
Apostolos Zormpas, Wilhelm Kley, Giovanni Picogna, and Barbara Ercolano
- Subjects
Physics ,Earth and Planetary Astrophysics (astro-ph.EP) ,education.field_of_study ,Radiative cooling ,010308 nuclear & particles physics ,Gas giant ,Population ,Giant planet ,FOS: Physical sciences ,Astronomy and Astrophysics ,Astrophysics ,01 natural sciences ,Accretion (astrophysics) ,13. Climate action ,Space and Planetary Science ,Planet ,0103 physical sciences ,Radiative transfer ,Astrophysics::Earth and Planetary Astrophysics ,education ,Pebble ,010303 astronomy & astrophysics ,Astrophysics::Galaxy Astrophysics ,Astrophysics - Earth and Planetary Astrophysics - Abstract
The solid accretion rate, necessary to grow gas giant planetary cores within the disk lifetime, has been a major constraint for theories of planet formation. We tested the solid accretion rate efficiency on planetary cores of different masses embedded in their birth disk, by means of 3D radiation-hydrodynamics, where we followed the evolution of a swarm of embedded solids of different sizes. We found that using a realistic equation of state and radiative cooling, the disk at 5 au is able to cool efficiently and reduce its aspect ratio. As a result, the pebble isolation mass is reached before the core grows to 10 Earth masses, stopping efficiently the pebble flux and creating a transition disk. Moreover, the reduced isolation mass halts the solid accretion before the core reaches the critical mass, leading to a barrier to giant planet formation, and it explains the large abundance of super-Earth planets in the observed population., Published in A&A, 8 pages, 9 figures
- Published
- 2020