Limitation of atmospheric composition by combustion-explosion in exoplanetary atmospheres
John Lee Grenfell, Stefanie Gebauer, Mareike Godolt, Barbara Stracke,, Ralph Lehmann, Heike Rauer

TL;DR
This paper explores how combustion and explosion processes could limit atmospheric compositions on exoplanets, especially Super Earths, by analyzing chemical reactions and potential explosive limits involving H2, O2, CO, and CH4.
Contribution
It combines combustion theory with exoplanetary atmospheric science to identify conditions leading to atmospheric explosions and constraints on chemical compositions.
Findings
H2 and O2 can react rapidly to form water and hydrogen peroxide.
CO and O2 mixtures may reach explosive levels on mini gas planets.
Certain CH4 and O2 atmospheres could be near explosive thresholds on rocky planets.
Abstract
This work presents theoretical studies which combine aspects of combustion and explosion theory with exoplanetary atmospheric science. Super Earths could possess a large amount of molecular hydrogen depending on disk, planetary and stellar properties. Super Earths orbiting pre-main sequence-M-dwarf stars have been suggested to possess large amounts of O2 produced abiotically via water photolysis followed by hydrogen escape . If these two constituents were present simultaneously, such large amounts of H2 and O2 can react via photochemistry to form up to about 10 Earth oceans. In cases where photochemical removal is slow so that O2 can indeed build up abiotically, the atmosphere could reach the combustion explosion limit. Then, H2 and O2 react extremely quickly to form water together with modest amounts of hydrogen peroxide. These processes set constraints for H2 O2 atmospheric…
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