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...

Full description

Bibliographic Details
Main Authors: Lyons, J. R., Ono, Shuhei, Whitehill, Andrew Richard
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Format: Article
Language:en_US
Published: 2014
Online Access:http://hdl.handle.net/1721.1/85603
https://orcid.org/0000-0001-5996-8217
https://orcid.org/0000-0002-1348-9584

Internet

http://hdl.handle.net/1721.1/85603
https://orcid.org/0000-0001-5996-8217
https://orcid.org/0000-0002-1348-9584

Similar Items