CARBON DIOXIDE ON TITAN
dc.creator | Maguire, W. C. | en_US |
dc.creator | Hanel, R. | en_US |
dc.creator | Jennings, D. | en_US |
dc.creator | Kunde, V. G. | en_US |
dc.creator | Samuelson, R. | en_US |
dc.creator | Aikin, A. | en_US |
dc.creator | Yung, Y. | en_US |
dc.date.accessioned | 2007-08-31T14:12:36Z | |
dc.date.available | 2007-08-31T14:12:36Z | |
dc.date.issued | 1982 | en_US |
dc.identifier | 1982-RA-4 | en_US |
dc.identifier.uri | http://hdl.handle.net/1811/29199 | |
dc.description | $^{1}$R. Hanel. et. al., Science 212, 192 (1981). $^{2}$W.C. Maguire, et. al., Nature 292, 683 (1981). $^{3}$V.G. Kunde, et. al., Nature 292, 686 (1981). | en_US |
dc.description.abstract | The infrared spectra returned by Voyager 1 of the atmosphere of Titan Saturn's largest moon, have shown the presence of eleven gaseous molecular $species.^{1 2 3}$ All of these previously reported species are compounds of hydrogen, carbon, and nitrogen. We have now identified a feature in the Titan spectra at $657 cm^{-1}$ as being due to the $\nu_{2}$ Q-branch of carbon dioxide. The identification of $CO_{2}$ is based on frequency correspondence between observed spectra and laboratory measurements, and on the elimination of alternative species which might be present in Titan's atmosphere. A mole fraction of $7\times 10^{-10}$ has been determined for $CO_{2}$ from the $667 cm^{-1}$ feature. | en_US |
dc.format.extent | 70650 bytes | |
dc.format.mimetype | image/jpeg | |
dc.language.iso | English | en_US |
dc.publisher | Ohio State University | en_US |
dc.title | CARBON DIOXIDE ON TITAN | en_US |
dc.type | article | en_US |
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