A&A 439, 1205-1213 (2005)
DOI: 10.1051/0004-6361:20052841
Modeling the Jovian subnebula
I. Thermodynamic conditions and migration of proto-satellites
Y. Alibert1, O. Mousis1, 2 and W. Benz11 Physikalisches Institut, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland
e-mail: yann.alibert@phim.unibe.ch
2 Observatoire de Besançon, CNRS-UMR 6091, BP 1615, 25010 Besançon Cedex, France
(Received 8 February 2005 / Accepted 9 May 2005 )
Abstract
We have developed an evolutionary turbulent model of the Jovian
subnebula consistent with the extended core accretion formation model of Jupiter.
This model takes into account the vertical structure of the subnebula, as well as the evolution
of the surface density as given by an
-disk model and is used to calculate the thermodynamical conditions in the subdisk for different values of the viscosity parameter.
We show that the Jovian subnebula evolves in two different phases during its
lifetime. In the first phase, the subnebula is fed through its outer edge by
the solar nebula as long as it has not been dissipated. In the second phase,
the solar nebula has disappeared and the Jovian subdisk expands and gradually
clears with time as Jupiter accretes the remaining material. We also
demonstrate that early generations of satellites formed during the beginning
of the first phase of the subnebula cannot survive in this environment and
fall onto the proto-Jupiter. As a result, these bodies may contribute to
the enrichment of Jupiter in heavy elements. Moreover, migration
calculations in the Jovian subnebula allow us to follow the evolution of the
ices/rock ratios in the proto-satellites as a function of their migration
pathways. By tempting to reproduce the distance distribution of the Galilean
satellites, as well as their ices/rock ratios, we obtain some constraints
on the viscosity parameter of the Jovian subnebula.
Key words: planets and satellites: formation -- solar system: formation
© ESO 2005

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