Journal of Geophysical Research Atmospheres · 1994 · 145 citations · 48 references
Natural SciencesChemistryEarth SciencesAtmospheric ChemistryAtmospheric ScienceChemical KineticsAerosol ChemistryAerosol PhysicsAerosol ScienceAtmospheric Oxidation ProcessesParticulate MatterStratospheric ChemistryAerosol AcidityAerosol Chemical CompositionAerosol Composition EffectsAerosol Heterogeneous ReactionsAtmospheric Chemical ReactionsAtmospheric Reaction KineticsReaction Rate EquationsReaction Rate Modeling
We have measured the rate of reaction of N 2 O 5 with H 2 O on monodisperse, submicrometer H 2 SO 4 particles in a low‐temperature flow reactor. Measurements were carried out at temperatures between 225 K and 293 K on aerosol particles with sizes and compositions comparable to those found in the stratosphere. At 273 K, the reaction probability was found to be 0.103±0.006, independent of H 2 SO 4 composition from 64 to 81 wt %. At 230 K, the reaction probability increased from 0.077 for compositions near 60% H 2 S0 4 to 0.146 for compositions near 70% H 2 SO 4 . Intermediate conditions gave intermediate results except for low reaction probabilities of about 0.045 at 260 K on aerosols with about 78% H 2 SO 4 . The reaction probability did not depend on particle size. These results imply that the reaction occurs essentially at the surface of the particle. A simple model for this type of reaction that reproduces the general trends observed is presented. The presence of formaldehyde did not affect the reaction rate.
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John H. Perry · Journal of Chemical Education · 1950 · 3.8K citations
Joseph O. Hirschfelder · Journal of the American Chemical Society · 1956 · 1.2K citations