Fig. 13
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Partial pressures of most abundant species in the vapor calculated using the equilibrium method (left plot, same as Fig. B.3 from Charnoz et al. 2023) and the sum method (right plot, methodology of Zilinskas et al. 2023; Piette et al. 2023), for different monoatomic hydrogen pressure 
when the atmosphere is at equilibrium with the magma ocean at T = 3000 K and hydrogen is not in equilibrium with the magma ocean.
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