Mass independent oxygen isotopic composition of atmospheric sulfate: Origin and implications for the present and past atmosphere of earth and mars

被引:35
作者
Lee, CCW [1 ]
Savarino, J [1 ]
Thiemens, MH [1 ]
机构
[1] Univ Calif San Diego, Dept Chem, La Jolla, CA 92093 USA
关键词
D O I
10.1029/2000GL011826
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
It is reported that atmospheric (aerosol and rainwater! sulfate possesses a mass independent isotopic composition, with excess O-17. Laboratory experiments indicate that the oxidants, H2O2 and O-3, are the source of anomalous O-17 enrichments in atmospheric sulfate via aqueous phase S(IV) oxidation. The discovery of the oxygen anomaly in atmospheric sulfate, with definition of its origin, provides a new way to investigate atmospheric and general planetary processes. The observations provide new insight into atmospheric chemistry with application in studies of the evolution of the atmosphere and surface-atmosphere interactions, both on Earth and Mars.
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收藏
页码:1783 / 1786
页数:4
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