Molecular chlorine (Cl2) is an important yet poorly understood trace constituent of the lower atmosphere. Although a number of mechanisms have been proposed for the conversion of particle-bound chloride (Cl-) to gas-phase Cl2, the detailed processes involved remain uncertain.
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Links:
[1] http://admin.indiaenvironmentportal.org.in/feature-article/n2o5-oxidizes-chloride-cl2-acidic-atmospheric-aerosol
[2] http://admin.indiaenvironmentportal.org.in/category/author/hans-d-osthoff
[3] http://admin.indiaenvironmentportal.org.in/category/author/james-m-roberts
[4] http://admin.indiaenvironmentportal.org.in/category/author/steven-s-brown-et-al
[5] http://admin.indiaenvironmentportal.org.in/category/journal/science
[6] http://admin.indiaenvironmentportal.org.in/category/thesaurus/oxides-nitrogen-nox
[7] http://admin.indiaenvironmentportal.org.in/category/thesaurus/atmosphere-and-ozone-layer
[8] http://admin.indiaenvironmentportal.org.in/category/thesaurus/atmosphere
[9] http://admin.indiaenvironmentportal.org.in/category/thesaurus/aerosols
