Characterising face-on accretion onto and the subsequent contraction of protoplanetary discs

Autor: F.I. Pelupessy, S. Portegies Zwart, Onno R. Pols, T.P.G. Wijnen
Rok vydání: 2017
Předmět:
Angular momentum
Astronomy
FOS: Physical sciences
Astrophysics
01 natural sciences
Accretion disc
accretion
Planet
0103 physical sciences
planets and satellites: formation
010303 astronomy & astrophysics
GeneralLiterature_REFERENCE(e.g.
dictionaries
encyclopedias
glossaries)

planetary systems
Astrophysics::Galaxy Astrophysics
Solar and Stellar Astrophysics (astro-ph.SR)
Physics
Earth and Planetary Astrophysics (astro-ph.EP)
stars: formation
010308 nuclear & particles physics
Mathematics::Complex Variables
accretion disks
protoplanetary disks
Astronomy and Astrophysics
Dissipation
Planetary system
Astrophysics - Astrophysics of Galaxies
Accretion (astrophysics)
Ram pressure
Stars
Astrophysics - Solar and Stellar Astrophysics
13. Climate action
Space and Planetary Science
Astrophysics of Galaxies (astro-ph.GA)
Astrophysics::Earth and Planetary Astrophysics
Astrophysics - Earth and Planetary Astrophysics
Zdroj: Astronomy & Astrophysics, 602, A52
Astronomy & Astrophysics, 602, 1-18
Astronomy & Astrophysics
Astronomy & Astrophysics, 602, pp. 1-18
ISSN: 1432-0746
DOI: 10.48550/arxiv.1702.04383
Popis: Observations indicate that stars generally lose their protoplanetary discs on a timescale of about 5 Myr. Which mechanisms are responsible for the disc dissipation is still debated. Here we investigate the movement through an ambient medium as a possible cause of disc dispersal. The ram pressure exerted by the flow can truncate the disc and the accretion of material with no azimuthal angular momentum leads to further disc contraction. We derive a theoretical model from accretion disc theory that describes the evolution of the disc radius, mass, and surface density profile as a function of the density and velocity of the ambient medium. We test our model by performing hydrodynamical simulations of a protoplanetary disc embedded in a flow with different velocities and densities. We find that our model gives an adequate description of the evolution of the disc radius and accretion rate onto the disc. The total disc mass in the simulations follows the theoretically expected trend, except at the lowest density where our simulated discs lose mass owing to continuous stripping. This stripping may be a numerical rather than a physical effect. Some quantitative differences exist between the model predictions and the simulations. These are at least partly caused by numerical viscous effects in the disc and depend on the resolution of the simulation. Our model can be used as a conservative estimate for the process of face-on accretion onto protoplanetary discs, as long as viscous processes in the disc can be neglected. The model predicts that in dense gaseous environments, discs can shrink substantially in size and can, in theory, sweep up an amount of gas of the order of their initial mass. This process could be relevant for planet formation in dense environments.
Comment: Accepted for publication in A&A, 20 pages, 8 figures, 2 tables
Databáze: OpenAIRE