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arXiv 2403.03325astro-ph.EP
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JWST揭示一颗2倍地球半径的系外行星上富金属可混溶大气中存在CH$_4$、CO$_2$和H$_2$O

JWST Reveals CH$_4$, CO$_2$, and H$_2$O in a Metal-rich Miscible Atmosphere on a Two-Earth-Radius Exoplanet

Björn Benneke, Pierre-Alexis Roy, Louis-Philippe Coulombe, Michael Radica, Caroline Piaulet, Eva-Maria Ahrer, Raymond Pierrehumbert, Joshua Krissansen-Totton, H… 展开作者

Björn Benneke, Pierre-Alexis Roy, Louis-Philippe Coulombe, Michael Radica, Caroline Piaulet, Eva-Maria Ahrer, Raymond Pierrehumbert, Joshua Krissansen-Totton, Hilke E. Schlichting, Renyu Hu, Jeehyun Yang, Duncan Christie, Daniel Thorngren, Edward D. Young, Stefan Pelletier, Heather A. Knutson, Yamila Miguel, Thomas M. Evans-Soma, Caroline Dorn, Anna Gagnebin, Jonathan J. Fortney, Thaddeus Komacek, Ryan MacDonald, Eshan Raul, Ryan Cloutier, Lorena Acuna, David Lafrenière, Charles Cadieux, René Doyon, Luis Welbanks, Romain Allart

AI总结:

本研究利用JWST观测2.2倍地球半径的系外行星TOI-270d的透射光谱,发现其富金属可混溶大气含CH₄、CO₂等,提出亚海王星分类方案,推断其为岩质内核加少量吸积气体的可混溶包络亚海王星,或为该类行星典型代表。

摘要:

尽管亚海王星可能是行星形成最普遍的产物,但其本质仍知之甚少。尤其是半径在1.5-2.5$R_\bigoplus$(地球半径)的行星,其体密度可用差异极大的组成和内部结构同等合理地解释,从而导致对其形成过程的推断大相径庭。本文我们呈现了半径2.2$R_\bigoplus$的TOI-270d(质量4.78$M_\bigoplus$,平衡温度$T_\text{eq}$=350-380 K)的0.6-5.2$\boldsymbol{\u03bcm}$全波段JWST NIRISS/SOSS+NIRSpec/G395H透射光谱,为亚海王星范畴的大气表征提供了前所未有的灵敏度。我们检测到CH$_4$在1.15、1.4、1.7、2.3和3.3$\boldsymbol{\u03bcm}$处的5个振动带(置信度9.4$\boldsymbol{\u03c3}$)、CO$_2$在4.3$\boldsymbol{\u03bcm}$处的特征(4.8$\boldsymbol{\u03c3}$)、水蒸气(2.5$\boldsymbol{\u03c3}$),以及SO$_2$在4.0$\boldsymbol{\u03bcm}$处和CS$_2$在4.6$\boldsymbol{\u03bcm}$处的潜在特征。有趣的是,我们发现其整体大气高度富金属,平均分子量为$5.47_{-1.14}^{+1.25}$。我们推断其大气金属质量分数为$58_{-12}^{+8}\boldsymbol{\u0025}$,C/O比为$0.47_{-0.19}^{+0.16}$,表明外层包络约一半质量由高分子量挥发物(H$_2$O、CH$_4$、CO、CO$_2$)而非H$_2$/He构成。我们提出一种亚海王星分类方案,并将TOI-270d归类为“可混溶包络亚海王星”——其H$_2$/He与高分子量挥发物在可混溶的超临界富金属包络中充分混合。对于完全可混溶的包络,我们得出结论:TOI-270d的内部由$90_{-4}^{+3}$wt%(质量百分比)的岩石/铁构成,表明它最初是一颗岩质行星,后吸积了少量质量百分比的H$_2$/He,其整体包络金属含量可通过岩浆洋-包络反应解释,无需大量冰的吸积。TOI-270d很可能是整个亚海王星族群的一个典型代表。

英文摘要:

Even though sub-Neptunes likely represent the most common outcome of planet formation, their natures remain poorly understood. In particular, planets near 1.5-2.5$\,R_\oplus$ often have bulk densities that can be explained equally well with widely different compositions and interior structures, resulting in grossly divergent implications for their formation. Here, we present the full 0.6-5.2$\,μ\mathrm{m}$ JWST NIRISS/SOSS+NIRSpec/G395H transmission spectrum of the 2.2$\,R_\oplus$ TOI-270d ($4.78\,M_\oplus$, $T_\mathrm{eq}$=350-380 K), delivering unprecedented sensitivity for atmospheric characterization in the sub-Neptune regime. We detect five vibrational bands of CH$_4$ at 1.15, 1.4, 1.7, 2.3, and 3.3$\,μ$m (9.4$σ$), the signature of CO$_2$ at 4.3$\,μ$m (4.8$σ$), water vapor (2.5$σ$), and potential signatures of SO$_2$ at 4.0$\,μ\mathrm{m}$ and CS$_2$ at 4.6$\,μ\mathrm{m}$. Intriguingly, we find an overall highly metal-rich atmosphere, with a mean molecular weight of $5.47_{-1.14}^{+1.25}$. We infer an atmospheric metal mass fraction of $58_{-12}^{+8}\%$ and a C/O of $0.47_{-0.19}^{+0.16}$, indicating that approximately half the mass of the outer envelope is in high-molecular-weight volatiles (H$_2$O, CH$_4$, CO, CO$_2$) rather than H$_2$/He. We introduce a sub-Neptune classification scheme and identify TOI-270d as a "miscible-envelope sub-Neptune" in which H$_2$/He is well-mixed with the high-molecular-weight volatiles in a miscible supercritical metal-rich envelope. For a fully miscible envelope, we conclude that TOI-270d's interior is $90_{-4}^{+3}\,$wt$\,\%$ rock/iron, indicating that it formed as a rocky planet that accreted a few wt % of H$_2$/He, with the overall envelope metal content explained by magma-ocean/envelope reactions without the need for significant ice accretion. TOI-270d may well be an archetype of the overall population of sub-Neptunes.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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