Fig. 10

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Inferred posteriors for the most important internal structure parameters of TOI-396 b. The depicted parameters are the mass fractions of the inner core (wcore), mantle (wmantle) and envelope layers (wenvelope) with respect to the total planet mass, and the mass fraction of water in the envelope (Zenvelope). The top row shows the results when assuming a water prior motivated by a formation of the planet outside the iceline (case A), while the bottom row uses a water prior compatible with a formation inside the iceline (case B). At the same time, we run models with three different compositional priors for the planetary Si/Mg/Fe ratios: stellar (purple, option 1), iron-enriched compared to the star (pink, option 2) and sampled using a uniform prior (blue, option 3). The dotted lines show the prior distributions, while the dashed vertical lines show the median values of the posteriors.
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