1D atmospheric study of the temperate sub-Neptune K2-18b

被引:48
作者
Blain, D. [1 ]
Charnay, B. [1 ]
Bezard, B. [1 ]
机构
[1] Univ Paris, Sorbonne Univ, PSL Res Univ, LESIA,Observ Paris,CNRS, F-92195 Meudon, France
关键词
planets and satellites: atmospheres; infrared: planetary systems; planets and satellites: gaseous planets; molecular data; COLLISION-INDUCED ABSORPTION; HYDROGEN HALIDES; UPPER LIMITS; H-2; PAIRS; LINE LIST; MASS; PRESSURE; EXOPLANET; METHANE; SATURN;
D O I
10.1051/0004-6361/202039072
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Context. The atmospheric composition of exoplanets with masses between 2 and 10 M-circle plus is poorly understood. In that regard, the sub-Neptune K2-18b, which is subject to Earth-like stellar irradiation, offers a valuable opportunity for the characterisation of such atmospheres. Previous analyses of its transmission spectrum from the Kepler, Hubble (HST), and Spitzer space telescopes data using both retrieval algorithms and forward-modelling suggest the presence of H2O and an H-2-He atmosphere, but have not detected other gases, such as CH4.Aims. We present simulations of the atmosphere of K2-18 b using Exo-REM, our self-consistent 1D radiative-equilibrium model, using a large grid of atmospheric parameters to infer constraints on its chemical composition.Methods. We compared the transmission spectra computed by our model with the above-mentioned data (0.4-5 mu m), assuming an H-2-He dominated atmosphere. We investigated the effects of irradiation, eddy diffusion coefficient, internal temperature, clouds, C/O ratio, and metallicity on the atmospheric structure and transit spectrum.Results. We show that our simulations favour atmospheric metallicities between 40 and 500 times solar and indicate, in some cases, the formation of H2O-ice clouds, but not liquid H2O clouds. We also confirm the findings of our previous study, which showed that CH4 absorption features nominally dominate the transmission spectrum in the HST spectral range. We compare our results with results from retrieval algorithms and find that the H2O-dominated spectrum interpretation is either due to the omission of CH4 absorptions or a strong overfitting of the data. Finally, we investigated different scenarios that would allow for a CH4-depleted atmosphere. We were able to fit the data to those scenarios, finding, however, that it is very unlikely for K2-18b to have a high internal temperature. A low C/O ratio (approximate to 0.01-0.1) allows for H2O to dominate the transmission spectrum and can fit the data but so far, this set-up lacks a physical explanation. Simulations with a C/O ratio <0.01 are not able to fit the data satisfactorily.
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页数:20
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