论文标题
偏心碎屑带揭示了伴侣系外行星的动态历史
Eccentric debris belts reveal the dynamical history of the companion exoplanet
论文作者
论文摘要
近年来,在极性系统中已经观察到许多偏心碎屑带。它们形状的最常见解释是附近的怪异行星伴侣的存在。这种同伴的重力扰动将引起皮带中行星的周期性偏心变化,并具有一系列的进动频率。总体预期形状是一个具有有限最小宽度的偏心带。但是,已经发现几个观察到的偏心碎屑盘的宽度比理论期望较窄。在本文中,我们研究了可以产生这种宽度很小的两种机制:(i)原星盘可以与行星和/或行星相互作用,慢慢推动前者的偏心率并抑制后者的偏心率; (ii)伴侣行星本可以通过行星范围的散射来随机地获得偏心。我们表明,在适当的条件下,这两种情况都提供了一种合理的方式,可以减少偏心皮带外部的最小宽度到扰动行星的最小宽度。然而,由于气体缺乏和有限的盘寿命,在大分离(a> 10 au)下,原球盘的影响会减少。这些发现表明,人们可以使用碎屑盘的形状和宽度来揭示出极性系统的演变,从而限制原球面的特性和行星范围散射的流行率。对碎屑填充系统的进一步观察可以证实薄碎屑带是常见的情况,还是罕见的初始条件或进化过程的结果。
In recent years, a number of eccentric debris belts have been observed in extrasolar systems. The most common explanation for their shape is the presence of a nearby eccentric planetary companion. The gravitational perturbation from such a companion would induce periodic eccentricity variations on the planetesimals in the belt, with a range of precession frequencies. The overall expected shape is an eccentric belt with a finite minimum width. However, several observed eccentric debris discs have been found to exhibit a narrower width than the theoretical expectation. In this paper, we study two mechanisms that can produce this small width: (i) the protoplanetary disc can interact with the planet and/or the planetesimals, slowly driving the eccentricity of the former and damping the eccentricities of the latter; (ii) the companion planet could have gained its eccentricity stochastically, through planet-planet scatterings. We show that under appropriate conditions, both of these scenarios offer a plausible way to reduce the minimum width of an eccentric belt exterior to a perturbing planet. However, the effects of protoplanetary discs are diminished at large separations (a > 10 au) due to the scarcity of gas and the limited disc lifetime. These findings suggest that one can use the shape and width of debris discs to shed light on the evolution of extrasolar systems, constraining the protoplanetary disc properties and the prevalence of planet-planet scatterings. Further observations of debris-harbouring systems could confirm whether thin debris belts are a common occurrence, or the results of rare initial conditions or evolutionary processes.