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太阳系巨行星轨道结构的起源。

Origin of the orbital architecture of the giant planets of the Solar System.

作者信息

Tsiganis K, Gomes R, Morbidelli A, Levison H F

机构信息

Observatoire de la Côte d' Azur, CNRS, BP 4229, 06304 Nice Cedex 4, France.

出版信息

Nature. 2005 May 26;435(7041):459-61. doi: 10.1038/nature03539.

Abstract

Planetary formation theories suggest that the giant planets formed on circular and coplanar orbits. The eccentricities of Jupiter, Saturn and Uranus, however, reach values of 6 per cent, 9 per cent and 8 per cent, respectively. In addition, the inclinations of the orbital planes of Saturn, Uranus and Neptune take maximum values of approximately 2 degrees with respect to the mean orbital plane of Jupiter. Existing models for the excitation of the eccentricity of extrasolar giant planets have not been successfully applied to the Solar System. Here we show that a planetary system with initial quasi-circular, coplanar orbits would have evolved to the current orbital configuration, provided that Jupiter and Saturn crossed their 1:2 orbital resonance. We show that this resonance crossing could have occurred as the giant planets migrated owing to their interaction with a disk of planetesimals. Our model reproduces all the important characteristics of the giant planets' orbits, namely their final semimajor axes, eccentricities and mutual inclinations.

摘要

行星形成理论表明,巨行星在圆形且共面的轨道上形成。然而,木星、土星和天王星的偏心率分别达到了6%、9%和8%。此外,土星、天王星和海王星轨道平面相对于木星平均轨道平面的倾角最大值约为2度。现有的关于太阳系外巨行星偏心率激发的模型尚未成功应用于太阳系。在此我们表明,如果木星和土星越过它们1:2的轨道共振,一个具有初始准圆形、共面轨道的行星系统将演化到当前的轨道构型。我们表明,这种共振穿越可能发生在巨行星因与小行星盘相互作用而迁移时。我们的模型再现了巨行星轨道的所有重要特征,即它们最终的半长轴、偏心率和相互倾角。

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