A new pathway to SO: Revealing the NUV driven sulfur chemistry in hot gas giants
arXiv:2411.04781 · doi:10.1051/0004-6361/202450598
Abstract
Context. Photochemistry is a key process driving planetary atmospheres away from local thermodynamic equilibrium. Recent observations of the H dominated atmospheres of hot gas giants have detected SO as one of the major products of this process. Aims. We investigate which chemical pathways lead to the formation of SO in an atmosphere, and we investigate which part of the flux from the host star is necessary to initiate SO production. Methods. We use the publicly available S-N-C-H-O photochemical network in the VULCAN chemical kinetics code to compute the disequilibrium chemistry of an exoplanetary atmosphere. Results. We find that there are two distinct chemical pathways that lead to the formation of SO. The formation of SO at higher pressures is initiated by stellar flux >200 nm, whereas the formation of SO at lower pressures is initiated by stellar flux <200 nm. In deeper layers of the atmosphere, OH is provided by the hydrogen abstraction of HO, and sulfur is provided by the photodissociation of SH and S, which leads to a positive feedback cycle that liberates sulfur from the stable HS molecule. In higher layers of the atmosphere, OH is provided by the photodissociation of HO, and sulfur can be liberated from HS by either photodissociation of SH and S, or by the hydrogen abstraction of SH. Conclusions. We conclude that the stellar flux in the 200-350 nm wavelength range as well as the ratio of NUV/UV radiation are important parameters determining the observability of SO. In addition we find that there is a diversity of chemical pathways to the formation of SO. This is crucial for the interpretation of SO detections and derived elemental abundance ratios and overall metallicities.
Accepted for publication in Astronomy & Astrophysics
References in corpus (20)
- On the radiative equilibrium of irradiated planetary atmospheres
- Early Release Science of the exoplanet WASP-39b with JWST NIRSpec PRISM
- Atmospheric Sulfur Photochemistry on Hot Jupiters
- The Two Modes of Gas Giant Planet Formation
- Photochemically-produced SO in the atmosphere of WASP-39b
- A chemical model for the atmosphere of hot Jupiters
- VULCAN: an Open-Source, Validated Chemical Kinetics Python Code for Exoplanetary Atmospheres
- Tracing the formation history of giant planets in protoplanetary disks with Carbon, Oxygen, Nitrogen and Sulphur
- The ExoMolOP Database: Cross-sections and k-tables for Molecules of Interest in High-Temperature Exoplanet Atmospheres
- SO2, silicate clouds, but no CH4 detected in a warm Neptune
- The ARCiS framework for Exoplanet Atmospheres: Modelling Philosophy and Retrieval
- The ARCiS framework for Exoplanet Atmospheres: The Cloud Transport Model
- Stellar Wind Confinement of Evaporating Exoplanet Atmospheres and its Signatures in 1083 nm Observations
- VUV-absorption cross section of carbon dioxide from 150 to 800 K and applications to warm exoplanetary atmospheres
- Sulfur Chemistry in the Atmospheres of Warm and Hot Jupiters
- H2S and SO2 detectability in Hot Jupiters: Sulfur species as indicator of metallicity and C/O ratio
- Global Chemical Transport on Hot Jupiters: Insights from 2D VULCAN photochemical model
- Expanding the inventory of spectral lines used to trace atmospheric escape in exoplanets
- Day-night transport induced chemistry and clouds on WASP-39b I: Gas-phase composition
- Photodissociation and induced chemical asymmetries on ultra-hot gas giants. A case study of HCN on WASP-76 b