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Volumn 278, Issue 5344, 1997, Pages 1778-1780

Isotopic fractionation of stratospheric nitrous oxide

Author keywords

[No Author keywords available]

Indexed keywords

ISOTOPE; NITROGEN 15; NITROUS OXIDE; OXYGEN 18;

EID: 0030698728     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.278.5344.1778     Document Type: Review
Times cited : (153)

References (35)
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    • World Meteorological Organization, Scientific Assessment of Ozone Depletion: 1994, World Meteorological Organization, Global Ozone Research and Monitoring Project-Report 37 (World Meteorological Organization, Geneva, Switzerland, 1995).
    • (1995) Global Ozone Research and Monitoring Project-Report 37
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    • NASA Office of the Mission to Planet Earth, Science Division, Washington, DC
    • J. A. Kaye et al., NASA Reference Publication 1339 (NASA Office of the Mission to Planet Earth, Science Division, Washington, DC, 1994).
    • (1994) NASA Reference Publication 1339
    • Kaye, J.A.1
  • 24
    • 1842276337 scopus 로고    scopus 로고
    • note
    • +) electronic transition thought to be responsible for the continuum absorption, the shifts are similar to those reported in Table 1.
  • 26
    • 1842385036 scopus 로고    scopus 로고
    • note
    • 2O, respectively. Using the same formula to fit our model results, we obtain the corresponding enrichment factors of -15.4 and -13.2, in agreement with experimental values.
  • 28
    • 0016322177 scopus 로고
    • 2O would have a large impact on the photolysis rate of the molecule.
    • (1975) Rev. Geophys. Space Phys. , vol.13 , pp. 1
  • 30
    • 84944833370 scopus 로고
    • 2O isotopomers, exchange with O atoms is potentially important, although the activation energy for the exchange reaction is probably very high. Appropriate laboratory experiments should settle this question.
    • (1980) Geophys. Res. Left. , vol.7 , pp. 251
    • Cicerone, R.J.1    McCrumb, J.L.2
  • 35
    • 1842362997 scopus 로고    scopus 로고
    • note
    • We thank K. Boering, H. Craig, W. DeMore, R. Friedl, Y. Jiang, J. Kaye, T. Rahn, S. Sander, M. Thiemens, and M. Wahlen for valuable discussions and inputs. C.E.M. thanks the National Research Council for a NASA Jet Propulsion Laboratory Research Associateship. This research was supported in part by NASA grant NAG1-1806 to the California Institute of Technology.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.