ABSTRACT
We show that the escape of hydrogen from early Earth's atmosphere likely occurred at rates slower by two orders of magnitude than previously thought. The balance between slow hydrogen escape and volcanic outgassing could have maintained a hydrogen mixing ratio of more than 30%. The production of prebiotic organic compounds in such an atmosphere would have been more efficient than either exogenous delivery or synthesis in hydrothermal systems. The organic soup in the oceans and ponds on early Earth would have been a more favorable place for the origin of life than previously thought.
Subject(s)
Atmosphere , Earth, Planet , Hydrogen , Organic Chemicals/chemistry , Amino Acids/chemistry , Carbon Dioxide/chemistry , Diffusion , Electricity , Evolution, Chemical , Evolution, Planetary , Hydrogen/chemistry , Models, Theoretical , Oceans and Seas , Origin of Life , Photochemistry , Seawater , Temperature , Ultraviolet RaysABSTRACT
Simulation results of three-dimensional (3D) stationary magnetohydrodynamic (MHD) bow-shock flows around perfectly conducting spheres are presented. For strong upstream magnetic field a new complex bow-shock flow topology arises consisting of two consecutive interacting shock fronts. It is shown that the leading shock front contains a segment of intermediate 1-3 shock type. This is the first confirmation in 3D that intermediate shocks, which were believed to be unphysical for a long time, can be formed and can persist for small-dissipation MHD in a realistic flow configuration.