On the plasma chemistry of a cold atmospheric argon plasma jet with shielding gas device

dc.bibliographicCitation.articleNumber015005
dc.bibliographicCitation.firstPage015005
dc.bibliographicCitation.issue1
dc.bibliographicCitation.journalTitlePlasma Sources Science and Technology
dc.bibliographicCitation.volume25
dc.contributor.authorSchmidt-Bleker, Ansgar
dc.contributor.authorWinter, Jörn
dc.contributor.authorBösel, André
dc.contributor.authorReuter, Stephan
dc.contributor.authorWeltmann, Klaus-Dieter
dc.date.accessioned2025-02-27T12:55:47Z
dc.date.available2025-02-27T12:55:47Z
dc.date.issued2016
dc.description.abstractA novel approach combining experimental and numerical methods for the study of reaction mechanisms in a cold atmospheric Ar plasma jet is introduced. The jet is operated with a shielding gas device that produces a gas curtain of defined composition around the plasma plume. The shielding gas composition is varied from pure N2 to pure O2. The density of metastable argon Ar(4s,3 P ) 2 in the plasma plume was quantified using laser atom absorption spectroscopy. The density of long-living reactive oxygen and nitrogen species (RONS), namely O3, NO2, NO, N O2 , N2O5 and H2O2, was quantified in the downstream region of the jet in a multipass cell using Fourier-transform infrared spectroscopy (FTIR). The jet produces a turbulent flow field and features guided streamers propagating at several km s-1 that follow the chaotic argon flow pattern, yielding a plasma plume with steep spatial gradients and a time dependence on the ns scale while the downstream chemistry unfolds within several seconds. The fast and highly localized electron impact reactions in the guided streamer head and the slower gas phase reactions of neutrals occurring in the plasma plume and experimental apparatus are therefore represented in two separate kinetic models. The first electron impact reaction kinetics model is correlated to the LAAS measurements and shows that in the guided streamer head primary reactive oxygen and nitrogen species are dominantly generated from Ar(4s,3 P2). The second neutral species plug-flow model hence uses an Ar(4s,3 P2) source term as sole energy input and yields good agreement with the RONS measured by FTIR spectroscopy.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/18657
dc.identifier.urihttps://doi.org/10.34657/17676
dc.language.isoeng
dc.publisherBristol : IOP Publ.
dc.relation.doihttps://doi.org/10.1088/0963-0252/25/1/015005
dc.relation.essn1361-6595
dc.relation.issn0963-0252
dc.rights.licenseCC BY 3.0 Unported
dc.rights.urihttp://creativecommons.org/licenses/by/3.0
dc.subject.ddc530
dc.subject.otheratmospheric pressure plasmaeng
dc.subject.otherFourier-transform infrared spectroscopyeng
dc.subject.otherkinetic modelingeng
dc.subject.otherlaser atom absorption spectroscopyeng
dc.subject.otherplasma chemistryeng
dc.subject.otherplasma jeteng
dc.titleOn the plasma chemistry of a cold atmospheric argon plasma jet with shielding gas deviceeng
dc.typeArticle
dc.typeText
tib.accessRightsopenAccess
wgl.contributorINP
wgl.subjectPhysikger
wgl.typeZeitschriftenartikelger
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