Issue |
A&A
Volume 589, May 2016
|
|
---|---|---|
Article Number | A129 | |
Number of page(s) | 15 | |
Section | Planets and planetary systems | |
DOI | https://doi.org/10.1051/0004-6361/201527344 | |
Published online | 26 April 2016 |
Effect of turbulence on collisions of dust particles with planetesimals in protoplanetary disks
1
Laboratoire J.-L. Lagrange, Université Côte d’Azur, Observatoire de la Côte
d’Azur, CNRS,
06304
Nice,
France
e-mail:
holger.homann@oca.eu
2
Anton Pannekoek Institute for Astronomy, University of
Amsterdam, 1012
WX
Amsterdam, The
Netherlands
3
Department of Earth and Planetary Sciences, Tokyo Institute of
Technology, 152-8551
Tokyo,
Japan
4
Earth-Life Science Institute, Tokyo Institute of
Technology, 152-8550
Tokyo,
Japan
Received: 11 September 2015
Accepted: 29 January 2016
Context. Planetesimals in gaseous protoplanetary disks may grow by collecting dust particles. Hydrodynamical studies show that small particles generally avoid collisions with the planetesimals because they are entrained by the flow around them. This occurs when St, the Stokes number, defined as the ratio of the dust stopping time to the planetesimal crossing time, becomes much smaller than unity. However, these studies have been limited to the laminar case, whereas these disks are believed to be turbulent.
Aims. We want to estimate the influence of gas turbulence on the dust-planetesimal collision rate and on the impact speeds.
Methods. We used three-dimensional direct numerical simulations of a fixed sphere (planetesimal) facing a laminar and turbulent flow seeded with small inertial particles (dust) subject to a Stokes drag. A no-slip boundary condition on the planetesimal surface is modeled via a penalty method.
Results. We find that turbulence can significantly increase the collision rate of dust particles with planetesimals. For a high turbulence case (when the amplitude of turbulent fluctuations is similar to the headwind velocity), we find that the collision probability remains equal to the geometrical rate or even higher for St ≳ 0.1, i.e., for dust sizes an order of magnitude smaller than in the laminar case. We derive expressions to calculate impact probabilities as a function of dust and planetesimal size and turbulent intensity.
Key words: planets and satellites: formation / planet-disk interactions / turbulence / accretion, accretion disks / hydrodynamics / methods: numerical
© ESO, 2016
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