Origin of isotopic fractionation of terrestrial Xe: hydrodynamic fractionation during escape of the primordial H2-He atmosphere

Details Origin of isotopic fractionation of terrestrial Xe: hydrodynamic fractionation during escape of the primordial H2-He atmosphere Origin of isotopic fractionation of terrestrial Xe: hydrodynamic fractionation during escape of the primordial H2-He atmosphere

Aug 1988

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1988e%26psl..89..323s&link_type=abstract

Earth and Planetary Science Letters, Volume 89, Issue 3-4, p. 323-334.

Computer Science

23

Scientific paper

A systematic fractionation pattern of Xe isotopes of the terrestrial atmosphere can be explained by mixing of two components: hydrodynamically-fractionated Xe of the residual primordial atmosphere and isotopically-unfractionated Xe contained originally inside the Earth. The mixing model can also account for the absence of isotopic fractionation of Kr and Ar between meteorites and the Earth, as well as the difference of Xe patterns between meteorites and the Earth. The isotopic feature of terrestrial Ne also could be explained by hydrodynamic fractionation.

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