A numerical model was used to study methane photochemistry in the stratosphere of Neptune. The observed mixing ratio of methane, 2%, forces photolysis to occur near the CH 4 homopause. For an assumed nominal value of the eddy mixing coefficient of 10 6 cm 2 sec −1 at the CH 4 homopause, the predicted average mixing ratios of C 2H 6 and C 2H 2, 1.5 × 10 −6 and 6 × 10 −7, respectively, agree well with observations in the infrared. The acetylene and ethane abundances are weakly dependent upon the strength of the eddy mixing and directly proportional to it. Haze production from methane photochemistry results from the formation of hydrocarbon ices and polyacetylenes. The calculated mixing ratios of C 2H 6, C 2H 2 are large enough to cause condensation to their respective ices near the tropopause. These hazes are capable of providing the necessary aerosol optical depth at the appropriate pressure levels required by observations of Neptune in the visible and near IR. Polyacetylene formation from C 2H 2 photolysis is limited by the low quantum yield of dissociation for acetylene, efficient recycling of its photolysis products by the other hydrocarbons, and the greatly reduced solar flux at Neptune. Comparisons of model predictions to Uranus show both a lower ratio of polyacetylene production to hydrocarbon ice and a lower likelihood of UV postprocessing of the acetylene ice to polymers on Neptune compared to Uranus. This is in agreement with the observed difference in the single scattering albedo of the stratospheric aerosols in the visible between Uranus and Neptune, with the aerosols on Neptune being brighter.
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