Javascript must be enabled to continue!
Are the observed gaps in protoplanetary discs caused by growing planets?
View through CrossRef
ABSTRACT
Recent detailed observations of protoplanetary discs revealed a lot of substructures that are mostly ring like. One interpretation is that these rings are caused by growing planets. These potential planets are not yet opening very deep gaps in their discs. These planets instead form small gaps in the discs to generate small pressure bumps exterior to their orbits that stop the inflow of the largest dust particles. In the pebble accretion paradigm, this planetary mass corresponds to the pebble isolation mass, where pebble accretion stops and efficient gas accretion starts. We perform planet population synthesis via pebble and gas accretion including type-I and type-II migration. In the first stage of our simulations, we investigate the conditions necessary for planets to reach the pebble isolation mass and compare their position to the observed gaps. We find that in order to match the gap structures 2000ME in pebbles is needed, which would be only available for the most metal-rich stars. We then follow the evolution of these planets for a few Myr to compare the resulting population with the observed exoplanet populations. Planet formation in discs with these large amounts of pebbles results in mostly forming gas giants and only very little super-Earths, contradicting observations. This leads to the conclusions that either (i) the observed discs are exceptions, (ii) not all gaps in observed discs are caused by planets, or (iii) that we miss some important ingredients in planet formation related to gas accretion and/or planet migration.
Oxford University Press (OUP)
Title: Are the observed gaps in protoplanetary discs caused by growing planets?
Description:
ABSTRACT
Recent detailed observations of protoplanetary discs revealed a lot of substructures that are mostly ring like.
One interpretation is that these rings are caused by growing planets.
These potential planets are not yet opening very deep gaps in their discs.
These planets instead form small gaps in the discs to generate small pressure bumps exterior to their orbits that stop the inflow of the largest dust particles.
In the pebble accretion paradigm, this planetary mass corresponds to the pebble isolation mass, where pebble accretion stops and efficient gas accretion starts.
We perform planet population synthesis via pebble and gas accretion including type-I and type-II migration.
In the first stage of our simulations, we investigate the conditions necessary for planets to reach the pebble isolation mass and compare their position to the observed gaps.
We find that in order to match the gap structures 2000ME in pebbles is needed, which would be only available for the most metal-rich stars.
We then follow the evolution of these planets for a few Myr to compare the resulting population with the observed exoplanet populations.
Planet formation in discs with these large amounts of pebbles results in mostly forming gas giants and only very little super-Earths, contradicting observations.
This leads to the conclusions that either (i) the observed discs are exceptions, (ii) not all gaps in observed discs are caused by planets, or (iii) that we miss some important ingredients in planet formation related to gas accretion and/or planet migration.
Related Results
Dynamics of giant planets in protoplanetary discs
Dynamics of giant planets in protoplanetary discs
New instruments such as the ALMA interferometer and SPHERE on VLT allowed to obtain a large number of high-resolution images of protoplanetary discs. In these images, substructures...
Minimal viscosity discs lock pairs of giant planets in 2:1 resonance with stalled migration.
Minimal viscosity discs lock pairs of giant planets in 2:1 resonance with stalled migration.
<div>
<div>
<p>Planets form in protoplanetary discs and their interactions with the gas give rise to migration. For a long time, discs wer...
Multi-fluid hydrodynamical simulations of circumbinary planet formation via pebble accretion
Multi-fluid hydrodynamical simulations of circumbinary planet formation via pebble accretion
Context. Since the detection of the first known transiting circumbinary planet (CBP), Kepler-16b,by the Kepler mission, a total pf 14 CBPs have been detected, raising questions abo...
Interior dynamics of small-core and coreless exoplanets
Interior dynamics of small-core and coreless exoplanets
Since the first exoplanet detection in 1992, the study of exoplanets has received considerable attention. It is becoming apparent that the diversity of the general exoplanet popula...
Protoplanetary discs in the laboratory: the fate of icy pebbles undergoing sublimation
Protoplanetary discs in the laboratory: the fate of icy pebbles undergoing sublimation
Planet formation in protoplanetary discs is a process whereby the primitive solids that are initially of microscopic scale, must be converted into larger objects such as pebbles (m...
How external photoevaporation changes the chemical composition of the inner disc
How external photoevaporation changes the chemical composition of the inner disc
Stars mostly form in cluster environments, where neighbouring stars can have an influence on the evolution of the newly formed protoplanetary discs. Besides gravitational interacti...
Observing planetary gaps in the gas of debris disks
Observing planetary gaps in the gas of debris disks
Recent ALMA observations discovered consequent amounts (i.e., up to a few 10−1 M⊙) of CO gas in debris disks that were expected to be gas-free. This gas is in general estimated to ...
Potential long-term habitable conditions on planets with primordial H-He atmospheres.
Potential long-term habitable conditions on planets with primordial H-He atmospheres.
<p><strong>Introduction:</strong> Planets that retain a primordial, H-He dominated atmosphere can have hydrogen act as a greenhouse gas: t...

