By Ellis J. H.
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Extra info for The Chemical Activity of the Ions of Hydrochloric Acid Determined by Electromotive Force Measurements
In this chain, termination involves the loss of H02 and CH30 2 radicals through peroxide formation, and the termination is balanced by new initiation steps involving ozone photolysis. The chemical equations corresponding to the new steps on the right hand semicircle of figure 8 are H02 + NO ~ OH + N02 (24) CHP2 + NO ~ CH30 + N02 (38) CHP + O2 ~ HCHO+ H02 (39) HCHO+ hv ~ H HCO (40) H + O2 ~ H02 HCO + O2 ~ CO + (34) + H02 (41) The outstanding feature of these equations is the direct or indirect formation of H02 in reactions (39), (40) and (41), and the regeneration of OH from H0 2 in reaction (24).
Lt of stratospheric 32 ozone through chemical interactions and temperature feedback effects. Nevertheless, most calculations show that, even with the controls of the Montreal Protocol, ozone depletions of several percentage points might be expected by the middle of the next century, and without the Protocol depletions would exceed 10%. The models also indicate that there might also be substantial seasonal and latitudinal fluctuations. Many calculations suggest that there might already be some ozone depletion.
Nature 344:729-734 Roan SL (1989) Ozone crisis: John Wiley, Chichester the 15-year evolution of a sudden global emergency. Rowland FS, Isaksen ISA (1988) The changing atmosphere. John Wiley, Chichester Schwartz SE (1989) Science 243:753-762 Acid deposition: unraveling a regional phenomenon. Seinfeld JH (1989) Urban air pollution: state of the science. Science 243:745-752 Singh HB, Salas L, Viezee W (1986) The global distribution of peroxyacetyl nitrate. Nature, Lond. 321 :588-591 Solomon S (1988) The mystery of the Antarctic ozone "hole".