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Coexistence of CH4, CO2, and H2O in exoplanet atmospheres

2020/10/23 by P. Woitke, O. Herbort, Ch. Helling +4 · 26 citations
Physics and Astronomy · #Astronomy and Astrophysical Research #Astrophysics and Star Formation Studies #Atmosphere (unit) #Condensation #Exoplanet #Nitrogen #Outgassing #Stellar, planetary, and galactic studies #Type (biology) #astro-ph.EP

paper · pdf · doi:10.1051/0004-6361/202038870

published in Astronomy and Astrophysics 646, A43 (EDP Sciences) · accepted by A&A, 5 pages and 5 pages appendices, 10 figures, 3 tables

arxiv created 2020/10/23 · openalex created_date 2020/10/29 · openalex publication_date 2020/11/27 · arxiv updated 2021/02/10 · openalex updated_date 2026/08/05

Abstract

We propose a classification of exoplanet atmospheres based on their H, C, O, and N element abundances below about 600 K. Chemical equilibrium models were run for all combinations of H, C, O, and N abundances, and three types of solutions were found, which are robust against variations of temperature, pressure, and nitrogen abundance. Type A atmospheres contain H 2 O, CH 4 , NH 3 , and either H 2 or N 2 , but only traces of CO 2 and O 2 . Type B atmospheres contain O 2 , H 2 O, CO 2 , and N 2 , but only traces of CH 4 , NH 3 , and H 2 . Type C atmospheres contain H 2 O, CO 2 , CH 4 , and N 2 , but only traces of NH 3 , H 2 , and O 2 . Other molecules are only present in ppb or ppm concentrations in chemical equilibrium, depending on temperature. Type C atmospheres are not found in the Solar System, where atmospheres are generally cold enough for water to condense, but exoplanets may well host such atmospheres. Our models show that graphite (soot) clouds can occur in type C atmospheres in addition to water clouds, which can occur in all types of atmospheres. Full-equilibrium condensation models show that the outgassing from warm rock can naturally provide type C atmospheres. We conclude that type C atmospheres, if they exist, would lead to false positive detections of biosignatures in exoplanets when considering the coexistence of CH 4 and CO 2 , and suggest other, more robust non-equilibrium markers.

Citations