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TOI-1634 b: An Ultra-short-period Keystone Planet Sitting inside the M-dwarf Radius Valley
The Astronomical Journal ( IF 5.1 ) Pub Date : 2021-07-30 , DOI: 10.3847/1538-3881/ac0157
Ryan Cloutier 1 , David Charbonneau 1 , Keivan G. Stassun 2 , Felipe Murgas 3 , Annelies Mortier 4 , Robert Massey 5 , Jack J. Lissauer 6 , David W. Latham 1 , Jonathan Irwin 1 , Raphalle D. Haywood 7 , Pere Guerra 8 , Eric Girardin 9 , Steven A. Giacalone 10 , Pau Bosch-Cabot 8 , Allyson Bieryla 1 , Joshua Winn 11 , Christopher A. Watson 12 , Roland Vanderspek 13 , Stphane Udry 14 , Motohide Tamura 15, 16, 17 , Alessandro Sozzetti 18 , Avi Shporer 19 , Damien Sgransan 14 , Sara Seager 19, 20, 21 , Arjun B. Savel 10, 22 , Dimitar Sasselov 1 , Mark Rose 6 , George Ricker 13 , Ken Rice 23, 24 , Elisa V. Quintana 25 , Samuel N. Quinn 1 , Giampaolo Piotto 26 , David Phillips 1 , Francesco Pepe 14 , Marco Pedani 27 , Hannu Parviainen 3, 28 , Enric Palle 3, 28 , Norio Narita 16, 29, 30, 31 , Emilio Molinari 32 , Giuseppina Micela 33 , Scott McDermott 34 , Michel Mayor 14 , Rachel A. Matson 35 , Aldo F. Martinez Fiorenzano 27 , Christophe Lovis 14 , Mercedes Lpez-Morales 1 , Nobuhiko Kusakabe 16, 17 , Eric L. N. Jensen 36 , Jon M. Jenkins 6 , Chelsea X. Huang 19 , Steve B. Howell 6 , Avet Harutyunyan 27 , Gbor Fűrsz 19 , Akihiko Fukui 37, 38 , Gilbert A. Esquerdo 1 , Emma Esparza-Borges 28 , Xavier Dumusque 14 , Courtney D. Dressing 10 , Luca Di Fabrizio 27 , Karen A. Collins 1 , Andrew Collier Cameron 39 , Jessie L. Christiansen 40 , Massimo Cecconi 27 , Lars A. Buchhave 41 , Walter Boschin 3, 27, 28 , Gloria Andreuzzi 27, 42
Affiliation  

Studies of close-in planets orbiting M dwarfs have suggested that the M-dwarf radius valley may be well explained by distinct formation timescales between enveloped terrestrials and rocky planets that form at late times in a gas-depleted environment. This scenario is at odds with the picture that close-in rocky planets form with a primordial gaseous envelope that is subsequently stripped away by some thermally driven mass-loss process. These two physical scenarios make unique predictions of the rocky/enveloped transition’s dependence on orbital separation such that studying the compositions of planets within the M-dwarf radius valley may be able to establish the dominant physics. Here, we present the discovery of one such keystone planet: the ultra-short-period planet TOI-1634 b (P=0.989 days, $F=121{F}_{\oplus }$, ${r}_{p}={1.790}_{-0.081}^{+0.080}$ R ) orbiting a nearby M2 dwarf (K s =8.7, R s =0.450 R , M s =0.502 M ) and whose size and orbital period sit within the M-dwarf radius valley. We confirm the TESS-discovered planet candidate using extensive ground-based follow-up campaigns, including a set of 32 precise radial velocity measurements from HARPS-N. We measure a planetary mass of ${4.91}_{-0.70}^{+0.68}$ M , which makes TOI-1634 b inconsistent with an Earth-like composition at $5.9\sigma $ and thus requires either an extended gaseous envelope, a large volatile-rich layer, or a rocky composition that is not dominated by iron and silicates to explain its mass and radius. The discovery that the bulk composition of TOI-1634 b is inconsistent with that of Earth supports the gas-depleted formation mechanism to explain the emergence of the radius valley around M dwarfs with ${M}_{s}\lesssim 0.5$ M .



中文翻译:

TOI-1634 b:位于 M 矮星半径谷内的超短周期基石行星

对围绕 M 矮星运行的近距行星的研究表明,M 矮星半径谷可以通过在气体耗尽环境中晚期形成的被包裹的地球和岩石行星之间不同的形成时间尺度来很好地解释。这种情况与靠近岩石行星形成的原始气态包层的图片不一致,该包层随后被一些热驱动的质量损失过程剥离。这两种物理场景对岩石/包络过渡对轨道分离的依赖性做出了独特的预测,因此研究 M 矮星半径谷内的行星组成可能能够建立主导物理学。在这里,我们展示了一颗这样的基石行星的发现:超短周期行星 TOI-1634 b ( P =0.989 天, $F=121{F}_{\oplus }$,${r}_{p}={1.790}_{-0.081}^{+0.080}$ R ) 围绕附近的 M2 矮星 ( K s =8.7, R s =0.450 R , M s =0.502 M ) 运行,其大小和轨道周期位于 M 矮星半径谷内。我们使用广泛的地面后续活动确认了 TESS 发现的行星候选者,包括来自 HARPS-N 的一组 32 个精确的径向速度测量值。我们测量了M 的行星质量,这使得 TOI-1634 b 与在 ${4.91}_{-0.70}^{+0.68}$ $5.9\西格玛 $因此需要一个扩展的气体包层、一个大的富含挥发物的层,或者一个不以铁和硅酸盐为主的岩石成分来解释它的质量和半径。TOI-1634 b的整体组成与地球不一致的发现支持了气体耗尽的形成机制来解释${M}_{s}\lesssim 0.5$ M 矮星周围半径谷的出现。

更新日期:2021-07-30
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