Abstract
Biological production and consumption of sulfur gases include compounds such as H2S, methylsulfides (CH3SH, (CH3) 2S, (CH3S)2), methanesulfonate (CH3SO3H), sulfoxides (SO2), carbon disulfide (CS2) and carbonyl sulfide (COS). Only H2S, COS, SO2 and CH3SH are true gases under most environmental conditions, but other sulfur compounds, such as dimethylsulfide (DMS; (CH3)S), dimethyldisulfide (DMDS; (CH3S)2), CS2, and ethanethiol (ESH; C2H5SH) are liquids with vapor pressures which allow volatilization. Therefore, most of these sulfur compounds are gaseous and play a role in the global flux (estimated to be 210 Tg S y-1 Table 1) from aquatic and terrestrial environments to the atmosphere. There, these gases engage in various (photo)chemical reactions, often mediated by radicals such as OH, NO3 and IO (Plane 1989), and O3 (Lee and Zhou 1994). Chemical reactions yield methanesulfonate (MSA) , SO2 and SO4 2- (non-sea salt sulfate, nss). As in the sulfur cycle in the geosphere, atmospheric sulfur (S2- to S4+) is ultimately oxidized to sulfate (S 6+ ), and may return to the Earth’s surface by wet and dry deposition.
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Visscher, P.T. (1996). Microbial Turn-over of Volatile Sulfur Compounds. In: Murrell, J.C., Kelly, D.P. (eds) Microbiology of Atmospheric Trace Gases. NATO ASI Series, vol 39. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-61096-7_13
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DOI: https://doi.org/10.1007/978-3-642-61096-7_13
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