Unraveling the non-equilibrium chemistry of the temperate sub-Neptune K2-18 b
A. Y. Jaziri, O. Sohier, O. Venot, N. Carrasco

TL;DR
This study investigates the non-equilibrium atmospheric chemistry of the temperate sub-Neptune K2-18 b using JWST data, revealing high metallicity and C/O ratio, and emphasizing the importance of advanced modeling for understanding exoplanet atmospheres.
Contribution
It introduces a comprehensive non-equilibrium chemistry model applied to K2-18 b, refining atmospheric parameters and demonstrating the significance of non-equilibrium processes over flat spectrum models.
Findings
High metallicity (266^{+291}_{-104}) inferred
High C/O ratio (C/O > 2.1) at 2 sigma
Robust detection of methane (CH4)
Abstract
The search for habitable, Earth-like exoplanets faces major observational challenges due to their small size and faint signals. M-dwarf stars offer a promising avenue to detect and study smaller planets, especially sub-Neptunes-among the most common exoplanet types. K2-18 b, a temperate sub-Neptune in an M-dwarf habitable zone, has been observed with HST and JWST, revealing an H2-rich atmosphere with CH4 and possible CO2. Conflicting interpretations highlight the importance of non-equilibrium chemistry, which is critical for constraining atmospheric parameters like metallicity, C/O ratio, and vertical mixing (Kzz). This study explores the parameter space of metallicity, C/O ratio, and Kzz for K2-18 b using the non-equilibrium chemistry model FRECKLL and JWST data. We generated spectra from a 3D grid of models and compared them to observations to refine atmospheric constraints. A fixed…
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