论文标题
Coralie radial速度搜索周围进化的星星(级联)II。长周期大行星绕的三个红色巨人的地震质量
Coralie radial velocity search for companions around evolved stars (CASCADES) II. Seismic masses for three red giants orbited by long-period massive planets
论文作者
论文摘要
星际学的出现是精确表征单星的黄金路径,这自然导致与外界学领域的协同作用。如今,恒星质量,半径和年龄的恒星恒星的精确确定是开发专用软件和技术以实现这一目标的推动力。但是,随着各种方法的存在,很明显,它们都有优势和不便,并且技术的准确性,效率和鲁棒性之间存在权衡。我们旨在比较和讨论用于可用苔丝数据的系外星主红色巨星的各种建模技术。然后,使用地震建模的结果来研究行星系统的动力学进化和大气蒸发。我们详细研究将各种地震建模技术的鲁棒性,准确性和精度应用于TESS观察到的四个系外行星主持的红色巨人。我们讨论了全球地震指数的使用,单个径向频率的使用以及非辐射振荡的使用。在每种情况下,我们都会讨论建模技术的优势和不便。我们使用各种建模技术确定了由长周期木星样行星旋转的外部主持人红色巨星的精确质量。对于每个目标,我们还从平均密度反转的质量估计值以及GAIA和光谱数据的半径值之间提供了质量的估计值。我们表明,即使这些目标的进化范围超出了红色巨型分支的估计地震年龄,也没有观察到这些目标的吞噬或迁移。
The advent of asteroseismology as the golden path to precisely characterize single stars naturally led to synergies with the field of exoplanetology. Today, the precise determination of stellar masses, radii and ages for exoplanet-host stars is a driving force in the development of dedicated software and techniques to achieve this goal. However, as various approaches exist, it is clear that they all have advantages and inconveniences and that there is a trade-off between accuracy, efficiency, and robustness of the techniques. We aim to compare and discuss various modelling techniques for exoplanet-host red giant stars for which TESS data are available. The results of the seismic modelling are then used to study the dynamical evolution and atmospheric evaporation of the planetary systems. We study, in detail, the robustness, accuracy and precision of various seismic modelling techniques when applied to four exoplanet-host red giants observed by TESS. We discuss the use of global seismic indexes, the use of individual radial frequencies and that of non-radial oscillations. In each case, we discuss the advantages and inconveniences of the modelling technique. We determine precise and accurate masses of exoplanet-host red giant stars orbited by long-period Jupiter-like planets using various modelling techniques. For each target, we also provide a model-independent estimate of the mass from a mean density inversion combined with radii values from Gaia and spectroscopic data. We show that no engulfment or migration is observed for these targets, even if their evolution is extended beyond their estimated seismic ages up the red giant branch.