KOPRI Repository

Modelling iodine particle formation and growth from seaweed in a chamber

Cited 28 time in wos
Cited 30 time in scopus

Full metadata record

DC Field Value Language
dc.contributor.authorODowd-
dc.contributor.authorPrijola-
dc.contributor.authorSellegri-
dc.contributor.authorYoon, Y. J.-
dc.date.accessioned2018-03-20T13:51:47Z-
dc.date.available2018-03-20T13:51:47Z-
dc.date.issued2005-
dc.identifier.urihttps://repository.kopri.re.kr/handle/201206/6362-
dc.description.abstractA sectional atmospheric chemistry and aerosol dynamics box model (AEROFOR) was further developed and used to simulate ultra-fine particle formation and growth from seaweed in a chamber flushed with particle-free atmospheric air. In the model, thermodynamically stable clusters were formed by dimer nucleation of OIO vapour, whose precursor was assumed to be molecular I-2 emitted by seaweed. Fractal geometry of particles was taken into account. For the I-2 fluxes of (0.5-1.5) x 10(9) cm(-3) s(-1) the model predicted strong particle bursts, the steady state concentrations of I-2 vapour and particles larger than 3 nm were as high as 4 x 10(9)-1.2 x 10(10) cm(-3) and 5.0 x 10(6)-9.2 x 10(6) cm(-3) respectively. The steady state was reached in less than 150 s and the predicted growth rates of 3-6 nm particles varied in the range of 1.2-3.6 nm min(-1). Sensitivity of the size distribution against I2O3 cluster formation, an extra condensable vapour, the photolysis rate of the OIO vapour as well as against the density of (OIO)(n)-clusters was discussed. The modelled results were in good agreement with the chamber measurements performed during the BIOFLUX campaign in September, 2003, in Mace Head, Ireland, confirming that I-2 emissions and nucleation of iodine oxides can largely explain the coastal nucleation phenomenon.-
dc.languageEnglish-
dc.subjectGeochemistry & Geophysics-
dc.titleModelling iodine particle formation and growth from seaweed in a chamber-
dc.typeArticle-
dc.identifier.bibliographicCitationODowd, et al. 2005. "Modelling iodine particle formation and growth from seaweed in a chamber". <em>Environmental Chemistry</em>(4): 271-281.-
dc.citation.titleEnvironmental Chemistry-
dc.citation.number4-
dc.identifier.doi10.1071/EN05075-
dc.citation.startPage271-
dc.citation.endPage281-
dc.description.articleClassificationSCIE-
dc.description.jcrRateJCR 2003:0-
dc.subject.keywordIodine chemistry-
dc.subject.keywordaerosol formation-
dc.subject.keywordaerosol growth-
dc.identifier.localId2005-0130-
dc.identifier.scopusid2-s2.0-29144475538-
dc.identifier.wosid000235491800005-
Appears in Collections  
2004-2005, A Study on the Arctic Environmental Characteristics (04-05) / Lee, Bang Yong (PP04108, PE05007)
Files in This Item
There are no files associated with this item.

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.

Browse