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The Effect of Tidal Inflation Instability on the Mass and Dynamical Evolution of Extrasolar Planets with Ultrashort Periods

机译:潮汐膨胀不稳定性对超短周期太阳系外行星质量和动力学演化的影响

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We investigate the possibility of substantial inflation of short-period Jupiter-mass planets, as a result of their internal tidal dissipation associated with the synchronization and circularization of their orbits. We employ the simplest prescription based on an equilibrium model with a constant lag angle for all components of the tide. We show the following: (1) In the low-eccentricity limit, the synchronization of the planets' spin with their mean motion is established before tidal dissipation can significantly modify their internal structure. (2) However, above a critical eccentricity, which is a function of the planets' semimajor axis, tidal dissipation of energy during the circularization process can induce planets to inflate in size before their eccentricity is damped. (3) For moderate eccentricities, the planets adjust to stable thermal equilibria in which the rate of their internal tidal dissipation is balanced by the enhanced radiative flux associated with their enlarged radii. (4) For sufficiently large eccentricities, the planets swell beyond two Jupiter radii and their internal degeneracy is partially lifted. Thereafter, their thermal equilibria become unstable and they undergo runaway inflation until their radii exceed the Roche radius. (5) We determine the necessary and sufficient condition for this tidal inflation instability. (6) These results are applied to study short-period planets. We show that for young Jupiter-mass planets, with a period of less than 3 days, an initial radius of about 2RJ, and an orbital eccentricity greater than 0.2, the energy dissipated during the circularization of their orbits is sufficiently intense and protracted to inflate their sizes up to their Roche radii. (7) We estimate the mass-loss rate, the asymptotic planetary masses, and the semimajor axes for various planetary initial orbital parameters. The possibility of gas overflow through both inner (L1) and outer (L2) Lagrangian points for the planets with short periods or large eccentricities is discussed. (8) Planets with more modest eccentricity (0.3) and semimajor axis (0.03-0.04 AU) lose mass via Roche lobe overflow mostly through the inner Lagrangian (L1) point. As a result of the conservation of total angular momentum, these mass-losing planets migrate outward, such that their semimajor axes and Roche radii increase while their mass, eccentricity, and tidal dissipation rate decrease until the mass loss is quenched. (9) Based on these results, we suggest that the combined effects of self-regulated mass loss and tidally driven orbital evolution may be responsible for the apparent lack of giant planets with ultrashort periods 3 days. (10) Mass loss during their orbital circularization may also have caused the planets with periods in the range ~3-7 days to be less massive than long-period planets, which are not affected by the star-planet tidal interaction. (11) The accretion of the short-period planets' tidal debris can also lead to the surface layer contamination and metallicity enhancement of their host stars. (12) Among the planets with periods of 1-3 weeks today, some may have migrated outward and attained circular orbits while others may have preserved their initial eccentricity and semimajor axis. Therefore, planets with circular orbits are expected to coexist with those with eccentric orbits in this period range. (13) Gross tidal inflation of planets occurs on the timescale ~106 yr after their formation for a brief interval of ~105 yr. The relatively large sizes of their classical and weak-line T Tauri host stars increase the planets' transit probability. The inflated sizes of the tidally heated planets also increase the eclipse depth of such transit events. Thus, the tidal inflation and disruption of planets may be directly observable around classical and weak-line T Tauri stars.
机译:我们研究了短周期木星质量行星大量膨胀的可能性,这是由于它们的内部潮汐消散与轨道的同步和圆化有关。对于潮汐的所有组成部分,我们都基于具有恒定滞后角的平衡模型采用最简单的处方。我们显示以下内容:(1)在低偏心极限中,在潮汐耗散可以显着改变其内部结构之前,已建立了行星自转与平均运动的同步。 (2)但是,在临界偏心率之上(这是行星的半长轴的函数),在圆化过程中潮汐能的耗散会导致行星在其偏心率被衰减之前膨胀。 (3)对于偏心率适中的行星,它们会调整到稳定的热平衡状态,在这种状态下,其内部潮汐耗散率与与半径增大相关的增强的辐射通量得以平衡。 (4)对于足够大的偏心率,行星膨胀超过两个木星半径,并且其内部简并性得到了部分消除。此后,它们的热平衡变得不稳定,并且经历失控的膨胀,直到其半径超过罗氏半径。 (5)我们确定了这种潮汐膨胀不稳定的必要和充分条件。 (6)这些结果被用于研究短周期行星。我们表明,对于年轻的木星质量行星,周期小于3天,初始半径约为2RJ,轨道偏心率大于0.2,在其轨道圆化过程中耗散的能量足够强并且会膨胀它们的尺寸不超过罗氏半径。 (7)我们估计了各种行星初始轨道参数的质量损失率,渐近行星质量和半长轴。讨论了短周期或大偏心率的行星通过内(L1)和外(L2)拉格朗日点气体溢出的可能性。 (8)偏心率较小(<0.3)和半长轴(> 0.03-0.04 AU)的行星通过罗氏裂片溢流损失的质量主要通过内部拉格朗日(L1)点。由于总角动量的守恒,这些质量下降的行星向外迁移,以使它们的半长轴和罗氏半径增加,而质量,偏心率和潮汐耗散率减小,直到质量损失消失为止。 (9)根据这些结果,我们认为自我调节质量损失与潮汐驱动的轨道演化的综合作用可能是造成超短3天周期的巨型行星明显缺乏的原因。 (10)轨道圆化过程中的质量损失也可能导致周期约为3-7天的行星的质量小于长周期行星的质量,这不受恒星-行星潮汐相互作用的影响。 (11)短周期行星的潮汐碎片的积聚也可能导致其主恒星的表面层污染和金属性增强。 (12)在今天的1-3周周期的行星中,一些行星可能向外迁移并达到了圆形轨道,而另一些行星可能保留了它们的初始偏心率和半长轴。因此,在此周期范围内,具有圆形轨道的行星有望与具有偏心轨道的行星共存。 (13)行星的总潮汐膨胀发生在它们形成后约106年的时间范围内,短暂间隔约为105年。经典和弱线的T Tauri主恒星相对较大,增加了行星的传播概率。潮汐加热的行星膨胀的大小也增加了这种过境事件的月食深度。因此,在经典和弱线T Tauri恒星周围可以直接观察到潮汐膨胀和行星破裂。

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