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Coupled Evolution of Earth’s H2-rich Proto-atmosphere and Oxidized Magma Ocean: Efficient H2O Production through Dissolved H2 Transport and Atmospheric Buffering of the Magma Ocean Redox State

  • Authors: Tatsuya Yoshida, Kirara Arima, Naoki Terada, Takeshi Kuroda, Kiyoshi Kuramoto

Tatsuya Yoshida et al 2026 The Planetary Science Journal 7 .

  • Provider: AAS Journals

Caption: Figure 3.

Overturn time of the boundary layer at the magma ocean–atmosphere interface, calculated from Equation (36), as a function of (a) magma ocean viscosity and the corresponding surface temperature and (b) surface temperature and the corresponding pressure at the bottom of the magma ocean. Colors indicate different internal heat fluxes.

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