Weidenschilling S J, Marzari F
Planetary Science Institute, Tucson, Arizona 85705, USA.
Nature. 1996;384(6610):619-21. doi: 10.1038/384619a0.
The recent discoveries of massive planetary companions orbiting several solar-type stars pose a conundrum. Conventional models for the formation of giant planets (such as Jupiter and Saturn) place such objects at distances of several astronomical units from the parent star, whereas all but one of the new objects are on orbits well inside 1 AU; these planets must therefore have originated at larger distances and subsequently migrated inwards. One suggested migration mechanism invokes tidal interactions between the planet and the evolving circumstellar disk. Such a mechanism results in planets with small, essentially circular orbits, which appears to be the case for many of the new planets. But two of the objects have substantial orbital eccentricities, which are difficult to reconcile with a tidal-linkage model. Here we describe an alternative model for planetary migration that can account for these large orbital eccentricities. If a system of three or more giant planets form about a star, their orbits may become unstable as they gain mass by accreting gas from the circumstellar disk; subsequent gravitational encounters among these planets can eject one from the system while placing the others into highly eccentric orbits both closer and farther from the star.
最近发现有几颗类日恒星周围环绕着巨大的行星伴星,这带来了一个难题。形成巨行星(如木星和土星)的传统模型认为,此类天体位于距离母恒星若干天文单位的位置,而除了一个新发现的天体之外,其他所有新发现的天体都在1天文单位以内的轨道上;因此,这些行星必定起源于更远的距离,随后向内迁移。一种提出的迁移机制涉及行星与正在演化的星周盘之间的潮汐相互作用。这样一种机制会导致行星拥有小的、基本为圆形的轨道,许多新发现的行星似乎就是这种情况。但其中有两个天体具有显著的轨道偏心率,这很难与潮汐联系模型相协调。在此,我们描述一种行星迁移的替代模型,它能够解释这些较大的轨道偏心率。如果围绕一颗恒星形成了一个由三个或更多巨行星组成的系统,随着它们从星周盘吸积气体而质量增加,其轨道可能会变得不稳定;这些行星随后的引力相互作用会将其中一个行星从系统中弹出,同时将其他行星置于离恒星更近和更远的高度偏心轨道上。