Geophysical Research Letters · 1994 · 68 citations · 35 references
Natural SciencesChemistryEarth SciencesAtmospheric ChemistryAtmospheric SciencePhysical ChemistryAtmospheric Oxidation ProcessesHalogen ChemistryMarine Atmospheric ChemistryOzone ChemistryPhotochemical KineticsTropospheric ChemistryAtmospheric Nitrate FormationChlorine ChemistryChlorine Radical ChemistryHalogen Chemistry In The TroposphereKinetic Data AnalysisOzoneTropospheric Halogen ChemistryTropospheric Ozone Chemistry
We report here the first measurement of the reaction probability (ϕ) at 298 K for the reaction (1) HNO 3(g) + NaCl (s) → HCl (g) + NaNO 3(s) , ϕ = (4±2) × 10 −4 , which was determined using X‐ray photoelectron spectroscopy to follow the formation of nitrate on the surface of single crystals of NaCl. Along with recent kinetic data for the reaction N 2 O 5(g) + NaCl (s) → ClNO 2(g) + NaNO 3(s) , we show that in the dark with typical relative concentrations of N 2 O 5 and HNO 3 , the N 2 O 5 reaction should be competitive with, and may exceed, that of HNO 3 . The reactions of NO 2 and ClONO 2 with NaCl are expected to be much less important. Thus, the tropospheric production of chlorine atoms via photolysis of ClNO 2 from the N 2 O 5 reaction is anticipated, which has the potential to impact the ozone balance in the troposphere.
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