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arXiv 1208.0237astro-ph.SR
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Gliese 436行星系统的动力学演化:Kozai迁移是Gliese 436 b偏心率的潜在来源

Dynamical evolution of the Gliese 436 planetary system - Kozai migration as a potential source for Gliese 436b's eccentricity

Hervé Beust, Xavier Bonfils, Guillaume Montagnier, Xavier Delfosse, Thierry Forveille

摘要:

这颗靠近GJ 436的行星,由于其轨道周期非常短,轨道偏心率令人费解。考虑到星系的年龄,这颗行星应该在很久以前就已经潮汐循环了。近年来,人们提出了许多解释这一现象的尝试,要么涉及异常弱的潮汐,要么涉及遥远的伴星的扰动作用。我们在这里解决后一个问题的基础上Kozai迁移。我们认为,GJ 436 b以前位于更远离恒星,它经历了一个大规模的,倾斜的扰动通过Kozai机制引起的迁移。在这种情况下,伴星的扰动触发了GJ 436 b的高振幅变化,导致潮汐作用于近星点。然后轨道潮汐收缩到今天的位置。我们数值积分的三体系统包括潮汐和广义相对论修正。我们首先表明,从GJ 436 b的现今位置开始,不可避免地会导致Kozai振荡的衰减,并迅速使行星圆化。相反,从5-10倍远的地方开始允许Kozai周期的开始。潮汐作用在偏心率峰值阶段,并减少了行星的半长轴。最终结果是一个以两个阶段为特征的演化:第一个阶段是Kozai周期和缓慢收缩的半长轴,第二个阶段是一旦行星脱离Kozai共振,其特征是更快速的减少。在大多数情况下,这一过程的时间尺度似乎比行星的标准循环时间长得多,其系数大于50。该模型可以解决GJ 436 b的偏心率悖论。根据不同的轨道配置,GJ 436 b可能需要几个陀螺仪才能实现完全的轨道下降和圆化。根据这一设想,我们今天可能正在目睹设想的第二阶段,即半长轴已经减小,而偏心率仍然很大。然后,我们探索的参数空间,并得出在哪些条件下,这个模型可以是现实的系统的年龄。这就产生了对假定伴侣的特征的限制。

英文摘要:

The close-in planet orbiting GJ 436 presents a puzzling orbital eccentricity considering its very short orbital period. Given the age of the system, this planet should have been tidally circularized a long time ago. Many attempts to explain this were proposed in recent years, either involving abnormally weak tides, or the perturbing action of a distant companion. We address here the latter issue based on Kozai migration. We propose that GJ 436b was formerly located further away from the star and that it underwent a migration induced by a massive, inclined perturber via Kozai mechanism. In this context, the perturbations by the companion trigger high amplitude variations to GJ 436b that cause tides to act at periastron. Then the orbit tidally shrinks to reach its present day location. We numerically integrate the 3-body system including tides and General Relativity correction. We first show that starting from the present-day location of GJ 436b inevitably leads to damping the Kozai oscillations and to rapidly circularizing the planet. Conversely, starting from 5-10 times further away allows the onset of Kozai cycles. The tides act in peak eccentricity phases and reduce the semi-major axis of the planet. The net result is an evolution characterized by two phases: a first one with Kozai cycles and a slowly shrinking semi-major axis, and a second one once the planet gets out of the Kozai resonance characterized by a more rapid decrease. The timescale of this process appears in most cases much longer than the standard circularization time of the planet by a factor larger than 50. This model can provide a solution to the eccentricity paradox of GJ 436b. Depending on the various orbital configurations, it can take several Gyrs to GJ 436b to achieve a full orbital decrease and circularization. According to this scenario, we could be witnessing today the second phase of the scenario where the semi-major axis is already reduced while the eccentricity is still significant. We then explore the parameter space and derive in which conditions this model can be realistic given the age of the system. This yields constraints on the characteristics of the putative companion.

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