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Does nitrogen transport in vitreous silica only take place in molecular form?
KTH, Skolan för kemivetenskap (CHE), Kemi, Korrosionslära.
KTH, Skolan för kemivetenskap (CHE), Kemi, Korrosionslära.
2006 (Engelska)Ingår i: Journal of Applied Physics, ISSN 0021-8979, E-ISSN 1089-7550, Vol. 100, nr 10, s. 104904-Artikel i tidskrift (Refereegranskat) Published
Abstract [en]

It is generally believed that nitrogen transport in vitreous silica exclusively takes place in molecular form, although no evidence for this is found in the literature. Actually, an analysis of literature data of transport of nitrogen and noble gases in vitreous silica at 900 °C suggests it may not be the case. In order to clarify the operative species of nitrogen transport in this material, experiments of permeation and uptake/release have been performed with the use of gas phase analysis and isotopic labeling of nitrogen. By comparing the relative distributions of N2 14,14, N2 14,15, and N2 15,15 in exposure gas, permeated gas and released gas with distribution of equilibrated nitrogen molecules, the percentage of dissociated nitrogen in the transport has been evaluated at different temperatures. It has then been found that nitrogen undergoes dissociation not only on the surface of vitreous silica but also in its bulk and that the overall dissociation of nitrogen increases with temperature. It is concluded that nitrogen diffuses both in molecular and atomic forms with approximately 15% atomic nitrogen transport at 900 °C. The observed transport rates are explained by diffusion of molecular nitrogen combined with a retardation of dissociated nitrogen in reversible traps.

Ort, förlag, år, upplaga, sidor
2006. Vol. 100, nr 10, s. 104904-
Nyckelord [en]
Fused silica, Inert gases, Isotopes, Molecular structure, Thermal effects, Transport properties
Nationell ämneskategori
Kemi
Identifikatorer
URN: urn:nbn:se:kth:diva-7049DOI: 10.1063/1.2386937ISI: 000242408000107Scopus ID: 2-s2.0-33845221246OAI: oai:DiVA.org:kth-7049DiVA, id: diva2:11941
Anmärkning
QC 20100909Tillgänglig från: 2007-05-08 Skapad: 2007-05-08 Senast uppdaterad: 2017-12-14Bibliografiskt granskad

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