Temporal evolution of two runs with our (standard) choice of evaporation (solid) and for the classical choice where solids end up in the core (dashed). Other parameter are the same (e.g., Ṁ_Z = 10⁻⁵ M_⊕ yr⁻¹). Due to the absorption of vapor by the envelope and the concomitant reduction of the local pressure scaleheight, the intake of nebular gas (M_xy) speeds up in the run where pebbles sublimate.