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001 | 42749 | ||
005 | 20240712101045.0 | ||
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024 | 7 | _ | |a 2128/765 |2 Handle |
037 | _ | _ | |a PreJuSER-42749 |
041 | _ | _ | |a eng |
082 | _ | _ | |a 550 |
084 | _ | _ | |2 WoS |a Meteorology & Atmospheric Sciences |
100 | 1 | _ | |a Anttila, T. |b 0 |u FZJ |0 P:(DE-Juel1)VDB45939 |
245 | _ | _ | |a Modelling the formation of organic particles in the atmosphere |
260 | _ | _ | |a Katlenburg-Lindau |b EGU |c 2004 |
300 | _ | _ | |a 1071 - 1083 |
336 | 7 | _ | |a Journal Article |0 PUB:(DE-HGF)16 |2 PUB:(DE-HGF) |
336 | 7 | _ | |a Output Types/Journal article |2 DataCite |
336 | 7 | _ | |a Journal Article |0 0 |2 EndNote |
336 | 7 | _ | |a ARTICLE |2 BibTeX |
336 | 7 | _ | |a JOURNAL_ARTICLE |2 ORCID |
336 | 7 | _ | |a article |2 DRIVER |
440 | _ | 0 | |a Atmospheric Chemistry and Physics |x 1680-7316 |0 9601 |v 4 |
500 | _ | _ | |a Record converted from VDB: 12.11.2012 |
520 | _ | _ | |a Particle formation resulting from activation of inorganic stable clusters by a supersaturated organic vapour was investigated using a numerical model. The applied aerosol dynamic model included a detailed description of the activation process along with a treatment of the appropriate aerosol and gas-phase processes. The obtained results suggest that both gaseous sulphuric acid and organic vapours contribute to organic particle formation in continental background areas. The initial growth of freshly-nucleated clusters is driven mainly by condensation of gaseous sulphuric acid and by a lesser extent self-coagulation. After the clusters have reached sizes of around 2 nm in diameter, low-volatile organic vapours start to condense spontaneously into the clusters, thereby accelerating their growth to detectable sizes. A shortage of gaseous sulphuric acid or organic vapours limit, or suppress altogether, the particle formation, since freshly-nucleated clusters are rapidly coagulated away by pre-existing particles. The obtained modelling results were applied to explaining the observed seasonal cycle in the number of aerosol formation events in a continental forest site. |
536 | _ | _ | |a Chemie und Dynamik der Geo-Biosphäre |c U01 |2 G:(DE-HGF) |0 G:(DE-Juel1)FUEK257 |x 0 |
588 | _ | _ | |a Dataset connected to Web of Science |
650 | _ | 7 | |a J |2 WoSType |
700 | 1 | _ | |a Kerminen, V.-M. |b 1 |0 P:(DE-HGF)0 |
700 | 1 | _ | |a Kulmala, M. |b 2 |0 P:(DE-HGF)0 |
700 | 1 | _ | |a Laaksonen, A. |b 3 |0 P:(DE-HGF)0 |
700 | 1 | _ | |a O'Dowd, C. |b 4 |0 P:(DE-HGF)0 |
773 | _ | _ | |g Vol. 4, p. 1071 - 1083 |p 1071 - 1083 |q 4<1071 - 1083 |0 PERI:(DE-600)2069847-1 |t Atmospheric chemistry and physics |v 4 |y 2004 |x 1680-7316 |
856 | 4 | _ | |u https://juser.fz-juelich.de/record/42749/files/59743.pdf |y OpenAccess |
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856 | 4 | _ | |u https://juser.fz-juelich.de/record/42749/files/59743.jpg?subformat=icon-180 |x icon-180 |y OpenAccess |
856 | 4 | _ | |u https://juser.fz-juelich.de/record/42749/files/59743.jpg?subformat=icon-640 |x icon-640 |y OpenAccess |
909 | C | O | |o oai:juser.fz-juelich.de:42749 |p openaire |p open_access |p driver |p VDB |p dnbdelivery |
913 | 1 | _ | |k U01 |v Chemie und Dynamik der Geo-Biosphäre |l Chemie und Dynamik der Geo-Biosphäre |b Environment (Umwelt) |0 G:(DE-Juel1)FUEK257 |x 0 |
914 | 1 | _ | |y 2004 |
915 | _ | _ | |0 StatID:(DE-HGF)0010 |a JCR/ISI refereed |
915 | _ | _ | |2 StatID |0 StatID:(DE-HGF)0510 |a OpenAccess |
920 | 1 | _ | |k ICG-II |l Troposphäre |d 31.12.2006 |g ICG |0 I:(DE-Juel1)VDB48 |x 0 |
970 | _ | _ | |a VDB:(DE-Juel1)59743 |
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980 | _ | _ | |a VDB |
980 | _ | _ | |a JUWEL |
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981 | _ | _ | |a I:(DE-Juel1)IEK-8-20101013 |
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