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Marine environment ozone depletion

Laturnus F, Svensson T, Wiencke C, Oberg G (2004) Ultraviolet radiation affects emission of ozone-depleting substances by marine macroalgae results from a laboratory incubation study. Environ Sci Technol 38 6605-6609... [Pg.268]

The chlorine chemistry is too slow for ozone depletion in the troposphere but bromine and, in particular, iodine provide - combining with heterogeneous chemistry (see below) - lead to ozone depletion in marine environments by the following catalytic cycles (Barrie and Platt 1995, Platt and Mortgaat 1999) A 5.398 < 5 10 cm molecule" s ... [Pg.578]

Whereas the role of halogens in the depletion of stratospheric ozone has been studied for several decades, the role of halogens in tropospheric O3 reactions in marine and polar environments has only been studied in the past 15 years. The competitive fate of halogen atoms (F, Cl, Br and I) is their reaction with ozone 5.388 = 1-2 10 cm molecule" s" . [Pg.577]

Monahan, E. C., D. E. Spiel and K. L. Davidson (1986) A model of marine aerosol generation via whitecaps and wave disruption in oceanic whitecaps. In Oceanic whitecaps and their role in air-sea exchange processes (Eds. E. C. Monahan and G. M. Niocaill), D. Reidel Publishing, Dordrecht, Holland, pp. 167-174 Montreal Protocol on Substances that Deplete the Ozone Layer (2000) United Nations Environment Programme, Nairobi (Kenia), 48 pp. [Pg.661]


See other pages where Marine environment ozone depletion is mentioned: [Pg.3]    [Pg.1937]    [Pg.359]    [Pg.549]    [Pg.552]    [Pg.648]    [Pg.131]    [Pg.327]    [Pg.102]    [Pg.7]   
See also in sourсe #XX -- [ Pg.74 ]




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