Early formation of a water ocean as a function of initial CO2 and H2O contents in a solidifying rocky planet
Helene Massol,
Anne Davaille,
Philippe Sarda
et al.
Abstract:We present a numerical model of a cooling magma ocean (MO) and the atmosphere degassing from it. The solidification of the MO leads to the enrichment of the silicate melt in volatiles, thus favoring degassing. Both reservoirs interact via heat and volatile exchange, where the volatiles are H2O and CO2. The aim of this model is to explore the influence of the atmosphere on the surface conditions after the MO stage, and especially the conditions required for the condensation o… Show more
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