Planet formation: Dust aggregation model versus a new hypothesis

Michael Wilkinson

Open University, Dep. Mathematics and Statistics, Milton Keynes, UK

The standard model for planet formation involves the aggregation of dust particles in a circumstellar accretion disc. It is surmised that the gas in the accretion disc must be turbulent in order to explain the relatively short lifetime of the disc. This makes it necessary to understand the dynamics of dust particles in a turbulent gas. I will review some basic properties of turbulent flows, and describe some recent results on the relative velocities and collision rates particles. I shall also describe how the properties of the gas in the circumstellar accretion disc can be estimated from a steady-state theory with very few input parameters. The dust particles are bound by van der Waals and other weak electrostatic forces. I will describe some estimates for the collision speed at which aggregates of dust particles will be fragmented, and show that the relative speeds of colliding dust aggregates make them very vulnerable to disruption. This is a strong indication that an alternative theory must be sought.

I shall describe an alternative hypothesis for the formation of planets, developed in collaboration with Bernhard Mehlig, which we term Concurrent Collapse. According to our hypothesis, when a cloud of interstellar gas collapses to form a star, it fragments, giving rise to smaller objects which are gravitationally bound to the star. These 'juvenile planets' are initially formed in non-circular orbits and have an elemental composition which is representative of the star. The juvenile planets can interact with the accretion disc in such a way that their orbit and their composition can be dramatically changed. Collisions between juvenile planets are also possible. Our hypothesis avoids having to resolve the difficulties faced by the dust aggregation model. It also provides satisfying explanations for the existence of exoplanets with eccentric orbits, for the occurrence of FU Orionis outbursts and for the melting of 'chondrules' found in meterorites.

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