Volume 413, Number 1, January I 2004
|Page(s)||373 - 380|
|Section||Planets and planetary systems|
|Published online||17 December 2003|
Modeling the thermodynamical conditions in the Uranian subnebula – Implications for regular satellite composition
CNRS-UMR 6091, Observatoire de Besançon, BP 1615, 25010 Besançon Cedex, France
Corresponding author: Olivier.Mousis@obs-besancon.fr
Accepted: 12 September 2003
We study the thermodynamical conditions existing in the Uranian subnebula from which the regular satellites were presumably formed, assuming it was produced by an earth-sized body impact on proto-Uranus (Stevenson [CITE]; Slattery et al. [CITE]). Two evolutionary turbulent models of the Uranian subnebula are constructed. Both are derived from the solar nebula analytical model of Dubrulle ([CITE]) and Drouart et al. ([CITE]). Each model provides a distinct chemical composition which depends on the assumed origin of the subdisk's material (proto-Uranus or impactor ejected material). Moreover, the evolution of the chemistry of C and N compounds is examined in order to assess the nature of major volatiles trapped into the ices of regular satellites. The temporal evolution of the D/H ratio in water is also explored in the Uranian subdisk, as a function of the gas phase composition. Such an analysis may provide constraints on the origin of the material which led to the formation of the regular satellite system.
Key words: planets and satellites: Uranus / solar system: formation / accretion, accretion disks
© ESO, 2004
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