Morbidelli A, Levison H F, Tsiganis K, Gomes R
Observatoire de la Côte d'Azur, BP 4229, 06304 Nice Cedex 4, France.
Nature. 2005 May 26;435(7041):462-5. doi: 10.1038/nature03540.
Jupiter's Trojans are asteroids that follow essentially the same orbit as Jupiter, but lead or trail the planet by an angular distance of approximately 60 degrees (co-orbital motion). They are hypothesized to be planetesimals that formed near Jupiter and were captured onto their current orbits while Jupiter was growing, possibly with the help of gas drag and/or collisions. This idea, however, cannot explain some basic properties of the Trojan population, in particular its broad orbital inclination distribution, which ranges up to approximately 40 degrees (ref. 8). Here we show that the Trojans could have formed in more distant regions and been subsequently captured into co-orbital motion with Jupiter during the time when the giant planets migrated by removing neighbouring planetesimals. The capture was possible during a short period of time, just after Jupiter and Saturn crossed their mutual 1:2 resonance, when the dynamics of the Trojan region were completely chaotic. Our simulations of this process satisfactorily reproduce the orbital distribution of the Trojans and their total mass.
木星的特洛伊小行星是一些小行星,它们基本上沿着与木星相同的轨道运行,但在与木星的角距离约60度处超前或落后于木星(共轨道运动)。据推测,它们是在木星附近形成的星子,在木星成长过程中被捕获到当前轨道,这一过程可能借助了气体阻力和/或碰撞。然而,这一观点无法解释特洛伊小行星群体的一些基本特性,特别是其广泛的轨道倾角分布,其范围可达约40度(参考文献8)。我们在此表明,特洛伊小行星可能在更遥远的区域形成,随后在巨行星通过清除相邻星子而迁移的时期被捕获到与木星的共轨道运动中。在木星和土星越过它们的1:2共振之后的短时间内,当特洛伊区域的动力学完全混乱时,捕获是可能的。我们对这一过程的模拟令人满意地再现了特洛伊小行星的轨道分布及其总质量。