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AbstractAbstract
[en] Fractionation of carbon isotopes in interstellar clouds is treated in some detail. Acting together, the exchange reaction 13C++12CO reversible 12C++13CO+ΔE and the high vapor pressure of CO may cause a preferential loss of 12C from the gas due to freezing onto dust grains. The 13C/12C ratio for the carbon in the gas is then raised by factors approximately 2 to 4. Fractionation of deuterium is also discussed since the proposed process is similar to the carbon isotope exchange and here there is no question that fractionation is a major effect. Important information about physical conditions in dense clouds - the fractional electron density and CO abundance - can be derived from the fractionation process producing the enhanced DCO+/HCO+ ratio. Possible fractionation reactions for isotopes of other elements (oxygen, sulfur) are mentioned briefly. (Auth.)
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Source
Audouze, J. (ed.) (Paris-11 Univ., 91 - Orsay (France). Centre de Spectrometrie Nucleaire et de Spectrometrie de Masse); International Astronomical Union; Astrophysics and Space Science Library Proceedings; v. 67; p. 105-114; ISBN 90-277-0807-X; ; 1977; D. Reidel; Dordrecht, Netherlands; International Astronomical Union session on CNO isotopes in astrophysics; Grenoble, France; 30 Aug 1976
Record Type
Book
Literature Type
Conference
Country of publication
ATOMIC IONS, CARBON COMPOUNDS, CARBON ISOTOPES, CARBON OXIDES, CHALCOGENIDES, CHARGED PARTICLES, COLLISIONS, EVEN-EVEN NUCLEI, EVEN-ODD NUCLEI, FLUIDS, GASES, ION COLLISIONS, IONS, ISOTOPES, LIGHT NUCLEI, MOLECULE COLLISIONS, NUCLEI, OXIDES, OXYGEN COMPOUNDS, SEPARATION PROCESSES, SPACE, STABLE ISOTOPES
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