Physics
Scientific paper
Dec 2004
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004agufm.p42a..02y&link_type=abstract
American Geophysical Union, Fall Meeting 2004, abstract #P42A-02
Physics
0300 Atmospheric Composition And Structure, 0305 Aerosols And Particles (0345, 4801), 0317 Chemical Kinetic And Photochemical Properties, 0343 Planetary Atmospheres (5405, 5407, 5409, 5704, 5705, 5707)
Scientific paper
It has been nearly a third of a century since Strobel¡¦s (1973) pioneering study of hydrocarbon chemistry and Axel¡¦s (1972) seminal work on the hydrocarbon aerosols. Methane, the parent molecule of hydrocarbons, is abundant on Titan. Photolysis of methane results in the synthesis of more complex hydrocarbons. The hydrocarbon chemistry is unique and rich and the same reactions apply to all reducing atmospheres. The hydrocarbon chemistry inevitably leads to the formation of high molecular weight products, giving rise to aerosols when the ambient atmosphere is cool enough for them to condense. We will review the progress in the hydrocarbon chemistry since the Voyager encounters (Yung et al., 1984). A number of pathways to organic synthesis from simple to complex hydrocarbons have been identified. Neutral schemes involve radicals such as C3H3 and C3H5. Ion schemes involve charged radicals such as c-C3H2+ and C4H3+. Both ringed and chained compounds can be synthesized. The organic chemistry is a very sensitive function of the H and H2 concentrations in the atmosphere. In fact, we can ``retrieve¡" the concentration of H atoms in the atmosphere from the recent ground-based observation of the allene to methylacetylene ratio. Preliminary results from Cassini will also be discussed.
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