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- bde65cfd-faec-4656-bc27-22dfe30912b7 definition "COS, a gas that is very stable and unreactive in the troposphere, but, it is thought, photolyzes to form carbon monoxide, CO, and sulfur, S, in the stratosphere. Through stratospheric chemical reactions, the sulfur atoms are converted to SO2 and H2SO4 which form sulfate aerosol, cloud condensation nuclei, but which eventually settles into the troposphere and reacts to form sulfuric acid, a component in acid rain. The major biospheric sources of COS are thought to be biological. [Analytical Chemistry; v 65; pages 976-982; 1993.] [Atmospheric Chemical Compounds: Sources, Occurrence, and Bioassay; Graedel, Hawkins, Claxton; page 513; 1986; Academic Press; Orlando.]" @default.
- bde65cfd-faec-4656-bc27-22dfe30912b7 id "1661635" @default.
- bde65cfd-faec-4656-bc27-22dfe30912b7 path_id 1eb0ea0a-312c-4d74-8d42-6f1ad758f999 @default.
- bde65cfd-faec-4656-bc27-22dfe30912b7 path_id b80a242d-d5f5-4a5f-976c-6f6fe2ab6b2c @default.
- bde65cfd-faec-4656-bc27-22dfe30912b7 path_id b9c56939-c624-467d-b196-e56a5b660334 @default.
- bde65cfd-faec-4656-bc27-22dfe30912b7 path_id c47f6052-634e-40ef-a5ac-13f69f6f4c2a @default.
- bde65cfd-faec-4656-bc27-22dfe30912b7 path_id e9f67a66-e9fc-435c-b720-ae32a2c3d8f5 @default.
- bde65cfd-faec-4656-bc27-22dfe30912b7 path_label "ATMOSPHERE" @default.
- bde65cfd-faec-4656-bc27-22dfe30912b7 path_label "ATMOSPHERIC CHEMISTRY" @default.
- bde65cfd-faec-4656-bc27-22dfe30912b7 path_label "EARTH SCIENCE" @default.
- bde65cfd-faec-4656-bc27-22dfe30912b7 path_label "SULFUR COMPOUNDS" @default.
- bde65cfd-faec-4656-bc27-22dfe30912b7 path_label "Science Keywords" @default.
- bde65cfd-faec-4656-bc27-22dfe30912b7 prefLabel "CARBONYL SULFIDE" @default.
- bde65cfd-faec-4656-bc27-22dfe30912b7 reference "Atmospheric and Air Chemistry Glossary from the Sam Houston State University. 'http://www.shsu.edu/~chemistry/Glossary/glos.html'" @default.
- bde65cfd-faec-4656-bc27-22dfe30912b7 tag "Science Keywords" @default.