Loyd R O Parke, Schreyer Ethan, Owen James E, Rogers James G, Broome Madelyn I, Shkolnik Evgenya L, Murray-Clay Ruth, Wilson David J, Peacock Sarah, Teske Johanna, Schlichting Hilke E, Duvvuri Girish M, Youngblood Allison, Schneider P Christian, France Kevin, Giacalone Steven, Batalha Natasha E, Schneider Adam C, Longo Isabella, Barman Travis, Ardila David R
Eureka Scientific, Oakland, CA, USA.
Imperial Astrophysics, Department of Physics, Imperial College London, London, UK.
Nature. 2025 Feb;638(8051):636-639. doi: 10.1038/s41586-024-08490-x. Epub 2025 Feb 12.
Exoplanet surveys have shown a class of abundant exoplanets smaller than Neptune on close, <100-day orbits. These planets form two populations separated by a natural division at about 1.8 R termed the radius valley. It is uncertain whether these populations arose from separate dry versus water-rich formation channels, evolved apart because of long-term atmospheric loss or a combination of both. Here we report observations of ongoing hydrogen loss from two sibling planets, TOI-776 b (1.85 ± 0.13 R) and TOI-776 c (2.02 ± 0.14 R), the sizes of which near the radius valley and mature (1-4 Gyr) age make them valuable for investigating the origins of the divided population of which they are a part. During the transits of these planets, absorption appeared against the Lyman-α emission of the host star, compatible with hydrogen escape at rates equivalent to 0.03-0.6% and 0.1-0.9% of the total mass per billion years of each planet, respectively. Observations of the outer planet, TOI-776 c, are incompatible with an outflow of dissociated steam, suggesting both it and its inner sibling formed in a dry environment. These observations support the strong role of hydrogen loss in the evolution of close-orbiting sub-Neptunes.
系外行星调查显示,存在一类数量丰富的系外行星,它们比海王星小,轨道周期短,小于100天。这些行星形成了两个群体,在半径约为1.8R处自然划分,这个区域被称为半径谷。目前尚不清楚这些群体是源于不同的干态与富水形成通道,还是由于长期大气损失而分化,亦或是两者兼而有之。在此,我们报告了对两颗姊妹行星TOI-776 b(半径为1.85±0.13R)和TOI-776 c(半径为2.02±0.14R)正在进行的氢损失观测。它们的大小接近半径谷,且年龄成熟(10亿至40亿年),这使得它们对于研究其所属的分化群体的起源具有重要价值。在这些行星凌日期间,宿主恒星的莱曼-α发射出现吸收现象,这与氢逃逸速率相符,分别相当于每颗行星每十亿年总质量的0.03%至0.6%和0.1%至0.9%。对外部行星TOI-776 c的观测结果与离解蒸汽外流不相符,这表明它及其内部姊妹行星都是在干燥环境中形成。这些观测结果支持了氢损失在近轨道亚海王星演化过程中的重要作用。