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. Author manuscript; available in PMC: 2019 Mar 4.
Published in final edited form as: Icarus. 2017 Jun 15;297:33–58. doi: 10.1016/j.icarus.2017.06.002

Figure 15:

Figure 15:

Partitioning of the oxygen-bearing vapor species in thermochemical equilibrium for a cometary composition grain (Lisse et al., 2007, see text) at the temperatures and pressures corresponding to the peak of the silicate ablation profile for Jupiter (Top left), Saturn (Top right), Uranus (Bottom left), Neptune (Bottom right).