Image Details

Choose export citation format:

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 5.

Mean H2 diffusion rate normalized by the hydrogen molecular number in the present-day terrestrial seawater (NTO), over the boundary layer overturn time. The solid lines represent the calculation results, and the dashed lines represent the analytical solution without chemical reactions described by Equation (42). The surface temperature is 2400 K, and the initial Fe3+/Fe2+ ratio is 0.08. Colors indicate different surface H2 partial pressures.

Other Images in This Article
Copyright and Terms & Conditions

Additional terms of reuse