Fig. 13
Influence of rock hydration on outgassing: the difference in the amounts of outgassed CO2 between dry and wet solidus melting temperatures are plotted versus planet mass for two different initial mantle temperatures Tinit (1600 K and 1800 K). The shown differences are comparisons between case 10 and the reference case (blue dots) as well as case 11 and 4 (red dots).
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