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Regional atmosphere alkanes

VPO reactions of typical alkanes may be considered conveniently in three temperature regions. Under some circumstances, particularly at pressures not greatly exceeding atmospheric, a curious and fundamentally important phenomenon known as the negative temperature coefficient (NTC) region is... [Pg.337]

Though most of the oxygen in the atmosphere has been formed by photosynthesis in plants, some is produced by photolysis of water vapour in the vacuum ultraviolet region A <200 nm. Photolysis of N2, NO, N02, NHa, CO, 002 and small aliphatic hydrocarbons (alkanes) set up complex reactions in the upper atmosphere. [Pg.224]

See other pages where Regional atmosphere alkanes is mentioned: [Pg.887]    [Pg.342]    [Pg.215]    [Pg.466]    [Pg.51]    [Pg.289]    [Pg.332]    [Pg.792]    [Pg.606]    [Pg.107]    [Pg.396]    [Pg.235]    [Pg.463]    [Pg.150]    [Pg.154]    [Pg.194]    [Pg.400]    [Pg.163]    [Pg.115]    [Pg.51]    [Pg.1299]    [Pg.1634]   
See also in sourсe #XX -- [ Pg.343 , Pg.344 ]



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Atmosphere, regions

Regional atmosphere

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