Photochemical modeling of CH 3 abundances in the outer solar system
Author(s) -
Lee Anthony Y. T.,
Yung Yuk L.,
Moses Julianne
Publication year - 2000
Publication title -
journal of geophysical research: planets
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/1999je001186
Subject(s) - uranus , neptune , titan (rocket family) , solar system , physics , gas giant , radiative transfer , planet , astrophysics , photochemistry , astrobiology , chemistry , exoplanet , quantum mechanics
Recent measurements of methyl radicals (CH 3 ) in the upper atmospheres of Saturn and Neptune by the Infrared Space Observatory (ISO) provide new constraints to photochemical models of hydrocarbon chemistry in the outer solar system. The derived column abundances of CH 3 on Saturn above 10 mbar and Neptune above the 0.2 mbar pressure level are (2.5–6.0) × 10 13 cm −2 and (0.7–2.8) × 10 13 cm −2 , respectively. We use the updated Caltech/Jet Propulsion Laboratory photochemical model, which incorporates hydrocarbon photochemistry, vertical molecular and bulk atmospheric eddy diffusion, and realistic radiative transfer modeling, to study the CH 3 abundances in the upper atmosphere of the giant planets and Titan. We identify the key reactions that control the concentrations of CH 3 in the model, such as the three‐body recombination reaction, CH 3 + CH 3 + M → C 2 H 6 + M. We evaluate and extrapolate the three‐body rate constant of this reaction to the low‐temperature limit (1.8×10 −16 T −3.75 e −300/ T , T <300 K) and compare methyl radical abundances in five atmospheres: Jupiter, Saturn, Uranus, Neptune, and Titan. The sensitivity of our models to the rate coefficients for the reactions H + CH 3 + M → CH 4 + M, H + C 2 H 3 → C 2 H 2 + H 2 , 1 CH 2 + H 2 → CH 3 + H, and H + C 2 H 5 → 2 CH 3 , the branching ratios of CH 4 photolysis, vertical mixing in the five atmospheres, and Lyman α photon enhancement at the orbit of Neptune have all been tested. The results of our model CH 3 abundances for both Saturn (5.1×10 13 cm −2 ) and Neptune (2.2×10 13 cm −2 ) show good agreement with ISO Short Wavelength Spectrometer measurements. Using the same chemical reaction set, our calculations also successfully generate vertical profiles of stable hydrocarbons consistent with Voyager and ground‐based measurements in these outer solar system atmospheres. Predictions of CH 3 column concentrations (for p ≤0.2 mbar) in the atmospheres of Jupiter (3.3×10 13 cm −2 ), Uranus (2.5×10 12 cm −2 ), and Titan (1.9×10 15 cm −2 ) may be checked by future observations.
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