Acetonitrile in the earth's atmosphere: An upper limit deduced from infrared solar spectra

dc.contributor.author	Muller, C.
dc.date	1985
dc.date.accessioned	2017-06-27T10:36:13Z
dc.date.available	2017-06-27T10:36:13Z
dc.identifier.uri	https://orfeo.belnet.be/handle/internal/5854
dc.description	An upper limit to the atmospheric acetonitrile mixing ratio of 3.2 X 10-1 is deduced from the high resolution Kitt Peak infrared atlas of the solar spectrum. The survey of the spectral region of CH3CN main absorption shows only stratospheric ozone lines and one water vapor line and does not permit any positive identification of acetonitrile.
dc.language	eng
dc.title	Acetonitrile in the earth's atmosphere: An upper limit deduced from infrared solar spectra
dc.type	Article
dc.subject.frascati	Earth and related Environmental sciences
dc.audience	Scientific
dc.source.title	Bulletin de la Classe des Sciences de l'Académie Royale de Belgique 5e Série
dc.source.volume	71
dc.source.issue	5
dc.source.page	225-229
Orfeo.peerreviewed	Yes
dc.identifier.doi	10.3406/barb.1985.61268