Fig. 5
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Example of the variation in CH3OH with time for L* = 100 L⊙ (left) and L* = 105 L⊙ (right). Lines are for the 100 parcels (full grid) from the center, color-coded by the temperature at t = 106 yr. The abundance of CH3OH decreases sharply at late times because of the reaction with neutral and ion species. For instance, at t = 5 × 105 yr, the most important destruction reactions are H3O+ + CH3OH → CH3OH2+ + H2O and H3+ + CH3OH → CH3+ + H2O + H2.
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