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Acetonitrile in the atmosphere

dc.contributor.authorBrasseur, G.
dc.contributor.authorArijs, E.
dc.contributor.authorDe Rudder, A.
dc.contributor.authorNevejans, D.
dc.contributor.authorIngels, J.
dc.date1983
dc.date.accessioned2017-06-28T12:18:16Z
dc.date.available2017-06-28T12:18:16Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/5907
dc.descriptionThe vertical distribution of acetonitrile between 0 and 55 km altitude is calculated assuming that CH3CN is released at the Earth's surface and that the main loss process in the stratosphere is the reaction with hydroxyl radicals. The influence of different possible surface concentrations is investigated. The role of the destruction of CH3CN by Cl, as well as the use of different eddy diffusion coefficients is briefly discussed. The results are compared with recent measurements of acetonitrile.
dc.languageeng
dc.titleAcetonitrile in the atmosphere
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.source.titleGeophysical Research Letters
dc.source.volume10
dc.source.issue8
dc.source.page725-728
Orfeo.peerreviewedYes
dc.identifier.doi10.1029/GL010i008p00725
dc.identifier.scopus2-s2.0-0020871337


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