论文标题

从开普勒91b的详细研究中对行星潮汐耗散的限制

Constraints on planetary tidal dissipation from a detailed study of Kepler 91b

论文作者

Fellay, L., Pezzotti, C., Buldgen, G., Eggenberger, P., Bolmont, E.

论文摘要

语境。随着数千个系外行星的检测,详细描述它们的动态演变代表了理解其形成的关键步骤。为了研究填充系统的物体之间发生的角动量的分布并研究轨道参数的演化,研究寄主恒星和行星中发生的潮汐的耗散是非常相关的。从理论的角度来看,可以通过依靠所谓的阶段或时间滞后平衡潮汐模型来研究潮汐的耗散模型,在这种模型中,降低了潮汐质量因子q'p,或者等效地在爱情数量和时间滞后(k2deltat)之间等效地描述了在范围内散布的有效诱导的范围。通过查看外部系统系统的当前配置来限制这些因素非常具有挑战性,并且拟定整个系统演变的模拟可能有助于阐明有关此过程的机制。目标。我们旨在通过研究开普勒91b的轨道演变来限制类似热jupiter行星的潮汐耗散因子。方法。首先,我们对开普勒-91进行了详细的Asteroseismc表征,并使用经典和星际异常约束计算了专用的恒星模型。然后,我们通过我们的轨道演化代码将恒星的演变与行星之一相结合,并通过考虑在行星和宿主星中消散的潮汐来研究系统的演变。结果。我们发现,K2DELTAT的最大值(或等效地,Q'p的最小值)确定在Kepler-91b中发生的平衡潮汐耗散的效率为0.4 pm 0.4 pm 0.25 s(4.5+5.8 * 10^5)。

Context. With the detection of thousands of exoplanets, characterising their dynamical evolution in detail represents a key step in the understanding of their formation. Studying the dissipation of tides occurring both in the host star and in the planets is of great relevance in order to investigate the distribution of the angular momentum occurring among the objects populating the system and to studying the evolution of the orbital parameters. From a theoretical point of view, the dissipation of tides throughout a body may be studied by relying on the so-called phase or time-lag equilibrium tides model in which the reduced tidal quality factor Q'p, or equivalently the product between the love number and the time lag (k2DeltaT), describe how efficiently tides are dissipated within the perturbed body. Constraining these factors by looking at the current configuration of the exoplanetary system is extremely challenging, and simulations accounting for the evolution of the system as a whole might help to shed some light on the mechanisms governing this process. Aims. We aim to constrain the tidal dissipation factors of hot-Jupiter-like planets by studying the orbital evolution of Kepler-91b. Methods. We firstly carried out a detailed asteroseismc characterisation of Kepler-91 and computed a dedicated stellar model using both classical and astereoseismic constraints. We then coupled the evolution of the star to the one of the planets by means of our orbital evolution code and studied the evolution of the system by accounting for tides dissipated both in the planet and in the host star. Results. We found that the maximum value for k2DeltaT (or equivalently the minimum value for Q'p) determining the efficiency of equilibrium tides dissipation occurring within Kepler-91b is 0.4 pm 0.25 s (4.5+5.8 * 10^5).

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