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. Author manuscript; available in PMC: 2019 May 1.
Published in final edited form as: Icarus. 2019 Jan 21;323:1–15. doi: 10.1016/j.icarus.2019.01.012

Figure 8.

Figure 8.

Comparison of the surface-integrated fluxes due to evaporation of a molten body half the mass of Pluto composed of E chondrite, excluding iron (E chondrite bulk composition projected into the CMAS composition space) and hydrodynamic escape of the resulting atmosphere. The cross-over pressure represents the steady-state pressure of the rock-vapor atmosphere surrounding the body.