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Detailed Reference Information |
Thiemens, M.H., Jackson, T., Mauersberger, K., Schueler, B. and Morton, J. (1991). Oxygen isotope fractionation in stratospheric CO2. Geophysical Research Letters 18: doi: 10.1029/91GL00121. issn: 0094-8276. |
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A new cryogenic collection system has been flown on board a balloon gondola to obtain separate samples of ozone and carbon dioxide without entrapping major atmospheric gases. Precision laboratory isotopic analysis of CO2 samples collected between 26 and 35.5 km show a mass-independent enrichment in both 17O and 18O of about 11 per mil (%) above tropospheric values. Ozone enrichment in its heavy isotopes was 9 to 16% in 50O3 and 8 to 11% in 49O3, respectively [Schueler et al., 1990>. A mechanism to explain the isotope enrichment in CO2 has been recently proposed by Yung et al. [1991>. Their model is based on the isotope exchange between CO2 and O3 via O(1D), resulting in a transfer of the ozone isotope enrichment to carbon dioxide. Predicted enrichments and measured values agree well. ¿American Geophysical Union 1991 |
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Abstract |
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Keywords
Planetology, Solid Surface Planets and Satellites, Atmospheric composition and chemistry, Planetology, Solid Surface Planets and Satellites, Instruments and techniques |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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