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Fig. B.2

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Comparison between the saturated vapor pressure and the gravitational pressure at 0.1 m and 1 m below the surface of a 100 km-sized planetesimal at different temperatures and for different molecules. The temperature down to 1 m below the surface is assumed to be the same as on the surface. The temperature needs to be about twice as high when considering H2O molecules than when considering CO2 molecules inorder for the vapor pressure to win over the gravitational pressure.

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