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Vacuum Ultraviolet Photochemistry. III. Primary Processes in the Vacuum Ultraviolet Photolysis of Water and Ammonia
98
Citations
8
References
1962
Year
Ultraviolet LightEngineeringAtmospheric PhotochemistryChemistryEnvironmental PhotochemistryChemical EngineeringHydrogen FormationHealth SciencesPhotochemistryPhotosystemsMechanistic PhotochemistryVacuum Ultraviolet PhotolysisPhysical ChemistryAmmoniaHydrogenUv-vis SpectroscopyVacuum Ultraviolet PhotochemistrySpectroscopyH AtomsPrimary ProcessesPrimary Photochemical ProcessChemical Kinetics
Water and ammonia have each been photolyzed in the absence and presence of C2D4 which served to scavenge H atoms. Wavelengths used were: for ammonia, 1849 and 1236 A; for water, 1236 A. Under conditions where H atoms are efficiently scavenged by C2D4, the production of H2 signifies a primary photochemical process giving molecular H2 directly. It is found that at 1849 A, ammonia decomposes almost entirely to H+NH2. At 1236 A, two primary processes are observed. (a)NH3→H2+NH,(b)NH3→H+NH2.Process (a) is about ⅙ as probable as process (b). At 1236 A, the photolysis of water proceeds via two primary processes. (c)H2O→H+OH,(d)H2O→H2+O.The probability of process (c) being three times that of process (d). It is suggested that primary process (d) constitutes a reasonable photochemical mechanism for hydrogen formation in the earth's upper atmosphere.
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