Fluxes Of Sulfur Compounds From Crops
Price
Free (open access)
Transaction
Volume
36
Pages
4
Published
1999
Size
321 kb
Paper DOI
10.2495/EURO990322
Copyright
WIT Press
Author(s)
Christopher Collins, Uwe Hoffmann, Uwe Kuhn , Anette Wolf and Juergen Kesselmeier
Abstract
Fluxes of Sulfur Compounds from Crops A contribution to BIATEX-2 Christopher Collins*, Uwe Hoffmann^, Uwe Kuhn , Anette Wolf and Juergen Kesselmeier^. 'I.C.C.E.T., Imperial College at Silwood Park, Ascot, Bekshire, U.K. SL5 7TE ^Max Planck Institute for Chemistry, Biogeochemistry Department, Joh.-J.-Becher-Weg 27, D-55128Mainz, Germany.Introduction The flux of sulfur gases to and from vegetation is one of the major uncertainties of the global sulfur cycle (Kesselmeier, 1991). Carbonyl sulfide (COS) is the principal sulfur gas in the atmosphere with a concentration of 500 ppt. Carbonyl sulfide has been proposed as an important climatic gas because it is a source of stratospheric submicron aerosol particles (Crutzen, 1976). The oceans are a major source of dimethyl sulfide ([CHs]2S)(DMS) (Andreae et al., 1985) as are rice paddy fields (Kanda et al., 1991). The other gaseous sulfur species of interest
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