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Tropospheric chemical reactivity

Tropospheric Chemical Reactivity and Its Consequences for Clean and Polluted Air... [Pg.64]

Trace-gas Lifetimes. The time scales for tropospheric chemical reactivity depend upon the hydroxyl radical concentration [HO ] and upon the rate of the HO/trace gas reaction, which generally represents the slowest or rate-determining chemical step in the removal of an individual, insoluble, molecular species. These rates are determined by the rate constant, e,g. k2s for the fundamental reaction with HO, a quantity that in general must be determined experimentally. The average lifetime of a trace gas T removed solely by its reaction with HO,... [Pg.81]

See other pages where Tropospheric chemical reactivity is mentioned: [Pg.65]    [Pg.66]    [Pg.67]    [Pg.69]    [Pg.71]    [Pg.73]    [Pg.75]    [Pg.77]    [Pg.81]    [Pg.83]    [Pg.85]    [Pg.89]    [Pg.91]    [Pg.93]    [Pg.95]    [Pg.97]    [Pg.99]    [Pg.101]    [Pg.103]    [Pg.107]    [Pg.111]    [Pg.115]   


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Troposphere

Tropospheric

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