Contribution of isotopologue self-shielding to sulfur mass-independent fractionation during sulfur dioxide photolysis

Contribution of isotopologue self-shielding to sulfur mass-independent fractionation during sulfur dioxide photolysis

Signatures of sulfur mass-independent fractionation (S-MIF) are observed for sulfur minerals in Archean rocks, and for modern stratospheric sulfate aerosols (SSA) deposited in polar ice. Ultraviolet light photolysis of SO[subscript 2] is thought to be the most likely source for these S-MIF signature...

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Bibliographic Details
Main Authors: Lyons, J. R. (Author), Ono, Shuhei (Contributor), Whitehill, Andrew Richard (Contributor)
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences (Contributor)
Format: Article
Language:English
Published: 2014-03-10T20:52:11Z.
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