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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Format: | Article |
Language: | English |
Published: |
2014-03-10T20:52:11Z.
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Online Access: | Get fulltext |