The influence of planetary engulfment on stellar rotation in metal-poor main-sequence stars

A. Oetjens, L. Carone, M. Bergemann, A. S. M. F. Astronomy, Ruprecht-Karls-Universitat Heidelberg, Institute for Space Sciences, Institut d'Estudis Espacials de Catalunya
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引用次数: 3

Abstract

The method of gyrochronology relates the age of its star to its rotation period. However, recent evidence of deviations from gyrochronology relations was reported in the literature. Here, we study the influence of tidal interaction between a star and its companion on the rotation velocity of the star, in order to explain peculiar stellar rotation velocities. The interaction of a star and its planet is followed using a comprehensive numerical framework that combines tidal friction, magnetic braking, planet migration, and detailed stellar evolution models from the GARSTEC grid. We focus on close-in companions from 1 to 20 M$_{Jup}$ orbiting low-mass, 0.8 and 1 M$_{\odot}$, main-sequence stars with a broad metallicity range from [Fe/H] = -1 to solar. Our simulations suggest that the dynamical interaction between a star and its companion can have different outcomes, which depend on the initial semi-major axis and the mass of the planet, as well as the mass and metallicity of its host star. In most cases, especially in the case of planet engulfment, we find a catastrophic increase in stellar rotation velocity from 1 kms$^{-1}$ to over 40 kms$^{-1}$, while the star is still on the main-sequence. The main prediction of our model is that low-mass main-sequence stars with abnormal rotation velocities should be more common at low-metallicity, as lower [Fe/H] favours faster planet engulfment, provided occurrence rate of close in massive planets is similar at all metallicities. Our scenario explains peculiar rotation velocities of low-mass main-sequence stars by the tidal interaction between the star and its companion. Current observational samples are too small and incomplete, and thus do not allow us to test our model.
贫金属主序星中行星吞噬对恒星旋转的影响
陀螺年代学的方法把它的恒星的年龄与它的自转周期联系起来。然而,最近文献报道了偏离陀螺年表关系的证据。在这里,我们研究了恒星及其伴星之间的潮汐相互作用对恒星旋转速度的影响,以解释特殊的恒星旋转速度。采用综合的数值框架,结合潮汐摩擦、磁制动、行星迁移和GARSTEC网格的详细恒星演化模型,跟踪恒星和行星之间的相互作用。我们关注的是1到20 M的近距离伴星,它们围绕着低质量、0.8和1 M的主序恒星运行,金属丰度范围从[Fe/H] = -1到太阳。我们的模拟表明,恒星与其伴星之间的动态相互作用可能会产生不同的结果,这取决于初始半长轴和行星的质量,以及其主恒星的质量和金属丰度。在大多数情况下,特别是在行星吞没的情况下,我们发现恒星的旋转速度从1公里$^{-1}$急剧增加到超过40公里$^{-1}$,而恒星仍在主序星上。我们模型的主要预测是,具有异常旋转速度的低质量主序恒星应该在低金属丰度下更常见,因为较低的[Fe/H]有利于更快的行星吞没,假设在所有金属丰度下大质量行星的发生率相似。我们的假设解释了低质量主序星的特殊旋转速度,这是由于恒星和伴星之间的潮汐相互作用。目前的观测样本太小且不完整,因此不允许我们测试我们的模型。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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