Search

Image Details

View Article Bookmark & Share

Choose export citation format:

Export Citation
Large resolution
Hi-Resolution Export to PDF

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 2.

Initial amounts of H2O (a) and H2 (b) as a function of the initial H2+H2O amount and the initial bottom pressure of the magma ocean in Case 1 described in Section 2.1. The amounts are normalized by the hydrogen molecular number in the present-day terrestrial seawater (NTO).

Other Images in This Article
Image in this article
Image in this article
Image in this article
Image in this article
Image in this article
Image in this article
Image in this article
Image in this article
Image in this article
Copyright and Terms & Conditions

Additional terms of reuse