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Fig. 4

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Example of a phase diagram Tdmx(P,xH2O$P,{x_{{{\rm{H}}_2}{\rm{O}}}}$) based on the shape of the 0.2 GPa isobar according to the experimental data (purple points) of Seward & Franck (1981). Higher isobars are obtained by shifting the 0.2 GPa curve vertically according to the given critical curve Tdmx(P, 0.5). Here, the V23 conv-1800 K case is shown. xA and xB show the coexisting particle fractions at 3 GPa and 1400 K. The waterpoor equilibrium abundance xA is used to compute the atmospheric abundance.

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