Fig. 4

Steady-state results for the fiducial parameters, for the simple model with single-seed evaporation (upper two panels) and many-seeds evaporation (lower two panels). a) Surface densities of ice, silicates and vapor (Σice, Σsil, and ΣZ, respectively) for the single-seed model. The silicates are locked in the icy pebbles outside the snowline, whereas they are bare grains interior to the snowline. b) Midplane pebbles-to-gas ratio ρpeb/ρgas, and pebbles-to-gas column density ratio Σpeb/ Σgas for the single-seed model. c) Same as panel a) but for the many-seeds model. The silicates are now divided in two populations: silicates that are locked up in icy pebbles (Σdirt), and free silicates (Σsil). Note that in panels a) and c) the x-axis ranges between r = 1.8 − 2.8au, for clarity. d) Same as b), but for the many-seeds model and with an additional line for the midplane “free silicates”-to-gas ratio ρsil/ρgas.
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