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Accueil du site > Divers > Pierre-Henri Chavanis > Hydrodynamics of Keplerian disks and planet formation

Hydrodynamics of Keplerian disks and planet formation

par Pierre-Henri Chavanis - 3 octobre 2006

Many astrophysical objects, ranging from young stars to massive black holes, are surrounded by widespread gaseous disks. The existence of a primordial disk around the sun was conjectured by Kant (1755) and Laplace (1796) in the 18th century to explain the quasi-circular, coplanar and prograd motion of the planets in the solar system. Such protoplanetary disks have recently been observed with the Hubble Space Telescope in the Orion nebula around stars less than one million years old. These gaseous disks can be considered as a by-product of the star formation : after the gravitational collapse of a molecular cloud, about 99% of the initial angular momentum is spread in an extended disk, while 99%of the mass forms the star, whose internal structure is hardly affected by rotation.

Whenever it has been possible to observe rotating, turbulent fluids with good resolution, it has been seen that individual, intense vortices form (Bengston \& Lighthill 1982 ; Hopfinger et al. 1983 ; Dowling and Spiegel 1990). One of the most striking example is Jupiter’s Great Red Spot, a huge vortex persisting for more than three centuries in the upper atmosphere of the planet. These coherent vortices are well reproduced in numerical simulations (McWilliams 1990, Marcus 1990) and laboratory experiments (Van Heist & Flor 1989, Sommeria, Meyers & Swinney 1988) of two-dimensional turbulence and their organization can be explained in terms of statistical mechanics (Miller 1990, Robert & Sommeria 1991, Sommeria et al. 1991, Chavanis & Sommeria 1998) . It seems therefore natural to expect their presence in accretion disks also (Dowling & Spiegel 1990, Abramowicz et al. 1992, Adams & Watkins 1995).

However, accretion disks are exceptional among rotating turbulent objects in the strong shears that these bodies are believed to possess and this shear might lead to rapid destruction of any structures that tend to form. This objection has been overruled by the numerical simulations of a two-dimensional flow in an external Keplerian shear by Bracco et al. (1998,1999) for an incompressible flow and Godon & Livio (1999a,b,c) for a compressible flow. Although cyclonic fluctuations are rapidely elongated and destroyed by the shear, anticyclonic vortices form and persist for a long time before being ultimately dissipated by viscosity. Naturally, this does not prove that coherent structures must form on disks, but this strengthens the argument that disks are likely to follow the norm of rotating, turbulent bodies. Other numerical results (Hunter & Horak 1983) and experimental work (Nezlin & Snezhkin 1993) comfort this point.

Coherent vortices in circumstellar disks can play an important role in the transport of dust particles and in the process of planet formation. Planets are thought to be formed from the dust grains embedded in the disk after a three-stage process : (i) in a first stage, microscopic particles suspended in the gas stick together on contact due to electrostatic or surface forces. When they reach sufficient sizes, they begin to sediment in the mid-plane of the disk due to the combined effect of the gravity and the friction with the gas. When settling dominates, a particle can grow by sweeping up smaller ones (Safronov 1969) and may easily reach sizes of several centimeters in a few thousand orbital periods (Weidenschilling & Cuzzi 1993). Bigger aggregates (>100 cm) are more difficult to form on relevant time scales because of collisional fragmentation (ii) When the layer of sedimented particles is sufficiently dense, the gravitational instability is triggered and the layer crumbles into numerous kilometer-sized bodies, the so-called ``planetesimals’’ (Safronov 1969, Goldreich & Ward 1973). (iii) The subsequent evolution is marked by planet’s growth due to the accumulation of planetesimals in successive collisions. This stage is well reproduced by dynamical models (Safronov 1969, Barge & Pellat 1991, 1993). When the solid core becomes sufficiently massive, it can accrete the surrounding gas and a giant planet, like Jupiter, is formed.

However, the above scenario faces two major problems. Recent studies have shown that circumstellar disks are relatively turbulent and that small-scale turbulence strongly reduces the sedimentation of the dust particles in the ecliptic plane (Weidenschilling 1980, Cuzzi et al. 1993, Dubrulle et al. 1995). For particles of relevant size, the density of the dust layer is not sufficient to overcome the threshold imposed by Jeans instability criterion. Therefore, the formation of the planetesimals, i.e. the passage from cm-sized to km-sized particles, is not clearly understood. In addition, it seems difficult, with the above model, to build up sufficiently massive cores in less than one million years before the gas has been swept away by the solar wind during the T-tauri phase (Safronov 1969, Wetherill 1988).

Both difficulties are ruled out if we allow for the presence of vortices in the disk. Their existence was first proposed by Von Weiz\"acker (1944) to explain the regularity of the planet distribution in the solar system : the famous Titius-Bode law (note that the idea of vortices in the solar system goes back to Descartes (1643)). This idea has been reintroduced recently by Barge & Sommeria (1995) and Tanga et al. (1996) who demonstrated that anticyclonic vortices in a rotating disk are able to capture and concentrate dust particles. The capture is made possible by the action of the Coriolis force which pushes the particles inward. These results are supported by a dynamical model which integrates the motion of the particles in the velocity field produced by a full Navier-Stokes simulation of the gas component Bracco et al. 1999, Godon & Livio 1999c). It is found that the particles are very efficiently captured and concentrated by the vortices. This is interesting because, without a confining mechanism, cm-sized bodies would rapidely fall onto the sun due to the inward drift associated with the velocity difference between gas and particles. Inside the vortices, the density of the dust cloud is increased by a large factor which is sufficient to trigger locally the gravitational instability and facilitate the formation of the planetesimals or the cores of giant planets. This trapping mechanism is quite rapid (a few rotations) and can reduce substantially the time scale of planet formation.