A&A 487, 265-270 (2008)
DOI: 10.1051/0004-6361:200809522
SPH simulations of grain growth in protoplanetary disks
G. Laibe1, J.-F. Gonzalez1, L. Fouchet2, and S. T. Maddison31 Université de Lyon, Lyon, 69003; Université Lyon 1, Villeurbanne, 69622; CNRS, UMR 5574, Centre de Recherche Astrophysique de Lyon; École Normale Supérieure de Lyon, 46 allée d'Italie, 69364 Lyon Cedex 07, France
e-mail: [Guillaume.Laibe;Jean-Francois.Gonzalez]@ens-lyon.fr
2 Institute of Astronomy, ETH Zürich, Schafmattstrasse 16, HPT D19, 8093 Zürich, Switzerland
e-mail: fouchet@phys.ethz.ch
3 Centre for Astrophysics and Supercomputing, Swinburne Institute of Technology, PO Box 218, Hawthorn, VIC 3122, Australia
e-mail: smaddison@swin.edu.au
Received 6 February 2008 / Accepted 5 June 2008
Abstract
Aims. In order to understand the first stages of planet formation, when tiny grains
aggregate to form planetesimals, one needs to simultaneously model grain
growth, vertical settling and radial migration of dust in protoplanetary disks.
In this study, we implement an analytical prescription for grain growth into a
3D two-phase hydrodynamics code to understand its effects on the dust
distribution in disks.
Methods. Following the analytic derivation of Stepinski & Valageas (1997, A&A, 319, 1007), which
assumes that grains stick perfectly upon collision, we implement a convenient
and fast method of following grain growth in our 3D, two-phase (gas+dust) SPH code. We then follow the evolution of the size and spatial distribution of a dust population in a classical T Tauri star disk.
Results. We find that the grains go through various stages of growth due to the
complex interplay between gas drag, dust dynamics, and growth. Grains
initially grow rapidly as they settle to the mid-plane, then experience a fast
radial migration with little growth through the bulk of the disk, and finally
pile-up in the inner disk where they grow more efficiently. This results in a
bimodal distribution of grain sizes. Using this simple prescription of grain
growth, we find that grains reach decimetric sizes in 105 years in the
inner disk and survive the fast migration phase.
Key words: planetary systems: protoplanetary disks -- hydrodynamics -- methods: numerical
© ESO 2008

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