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Fig. 2

image

Volatile chemical speciation in terms of outgassed mole fraction vs. oxygen fugacity of the mantle. The x-axis indicates the oxygen fugacity range in logarithmic units relative to the IW buffer. For reference (in log units), buffers QIF = IW-1, QFM = IW+3.8, and NiNiO = IW+4.2 approximately (Wood et al. 1990). From top to bottom: BOM, active MO phase, EOM and a steam-atmosphere phase that are characterized by different initial H/C between hydrogen and carbon. The corresponding input values of the initial volume mixing ratio of volatiles, surface pressures Ps, and temperatures Ts (Nikolaou et al. 2019) for the speciation model are indicated at the top of each panel.

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