001     22984
005     20240712100958.0
024 7 _ |2 DOI
|a 10.5194/acp-12-5113-2012
024 7 _ |2 WOS
|a WOS:000305281600020
024 7 _ |2 Handle
|a 2128/7597
037 _ _ |a PreJuSER-22984
041 _ _ |a eng
082 _ _ |a 550
084 _ _ |2 WoS
|a Meteorology & Atmospheric Sciences
100 1 _ |0 P:(DE-Juel1)144056
|a Ehn, M.
|b 0
|u FZJ
245 _ _ |a Gas phase formation of extremely oxidized pinene reaction products in chamber and ambient air
260 _ _ |a Katlenburg-Lindau
|b EGU
|c 2012
300 _ _ |a 5113 - 5127
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 |0 9601
|a Atmospheric Chemistry and Physics
|v 12
|x 1680-7316
|y 11
500 _ _ |a M. E. gratefully acknowledges financial support by the Emil Aaltonen foundation. This work was supported by the ERC Advanced Grant EU-FP7-ATMNUCLE (project no 227463), and by the Academy of Finland Center of Excellence program (project no 1118615).
520 _ _ |a High molecular weight (300-650 Da) naturally charged negative ions have previously been observed at a boreal forest site in Hyytiala, Finland. The long-term measurements conducted in this work showed that these ions are observed practically every night between spring and autumn in Hyytiala. The ambient mass spectral patterns could be reproduced in striking detail during additional measurements of alpha-pinene (C10H16) oxidation at low-OH conditions in the Julich Plant Atmosphere Chamber (JPAC). The ions were identified as clusters of the nitrate ion (NO3-) and alpha-pinene oxidation products reaching oxygen to carbon ratios of 0.7-1.3, while retaining most of the initial ten carbon atoms. Attributing the ions to clusters instead of single molecules was based on additional observations of the same extremely oxidized organics in clusters with HSO4- (Hyytiala) and C3F5O2- (JPAC). The most abundant products in the ion spectra were identified as C10H14O7, C10H14O9, C10H16O9, and C10H14O11. The mechanism responsible for forming these molecules is still not clear, but the initial reaction is most likely ozone attack at the double bond, as the ions are mainly observed under dark conditions. beta-pinene also formed highly oxidized products under the same conditions, but less efficiently, and mainly C-9 compounds which were not observed in Hyytiala, where beta-pinene on average is 4-5 times less abundant than alpha-pinene. Further, to explain the high O/C together with the relatively high H/C, we propose that geminal diols and/or hydroperoxide groups may be important. We estimate that the night-time concentration of the sum of the neutral extremely oxidized products is on the order of 0.1-1 ppt (similar to 10(6)-10(7) molec cm(-3)). This is in a similar range as the amount of gaseous H2SO4 in Hyytiala during day-time. As these highly oxidized organics are roughly 3 times heavier, likely with extremely low vapor pressures, their role in the initial steps of new aerosol particle formation and growth may be important and needs to be explored in more detail in the future.
536 _ _ |0 G:(DE-Juel1)FUEK491
|2 G:(DE-HGF)
|a Atmosphäre und Klima
|c P23
|x 0
588 _ _ |a Dataset connected to Web of Science
650 _ 7 |2 WoSType
|a J
700 1 _ |0 P:(DE-Juel1)129345
|a Kleist, E.
|b 1
|u FZJ
700 1 _ |0 P:(DE-HGF)0
|a Junninen, H.
|b 2
700 1 _ |0 P:(DE-HGF)0
|a Petäjä, T.
|b 3
700 1 _ |0 P:(DE-HGF)0
|a Lönn, G.
|b 4
700 1 _ |0 P:(DE-HGF)0
|a Schobesberger, S.
|b 5
700 1 _ |0 P:(DE-Juel1)VDB46017
|a Dal Maso, M.
|b 6
|u FZJ
700 1 _ |0 P:(DE-Juel1)129266
|a Trimborn, A.
|b 7
|u FZJ
700 1 _ |0 P:(DE-HGF)0
|a Kulmala, M.
|b 8
700 1 _ |0 P:(DE-HGF)0
|a Worsnop, D.
|b 9
700 1 _ |0 P:(DE-Juel1)16324
|a Wahner, A.
|b 10
|u FZJ
700 1 _ |0 P:(DE-Juel1)VDB1780
|a Wildt, J.
|b 11
|u FZJ
700 1 _ |0 P:(DE-Juel1)16346
|a Mentel, Th.F.
|b 12
|u FZJ
773 _ _ |0 PERI:(DE-600)2069847-1
|a 10.5194/acp-12-5113-2012
|g Vol. 12, p. 5113 - 5127
|p 5113 - 5127
|q 12<5113 - 5127
|t Atmospheric chemistry and physics
|v 12
|x 1680-7316
|y 2012
856 7 _ |u http://dx.doi.org/10.5194/acp-12-5113-2012
856 4 _ |u https://juser.fz-juelich.de/record/22984/files/FZJ-22984.pdf
|y OpenAccess
|z Published final document.
856 4 _ |u https://juser.fz-juelich.de/record/22984/files/FZJ-22984.jpg?subformat=icon-1440
|x icon-1440
|y OpenAccess
856 4 _ |u https://juser.fz-juelich.de/record/22984/files/FZJ-22984.jpg?subformat=icon-180
|x icon-180
|y OpenAccess
856 4 _ |u https://juser.fz-juelich.de/record/22984/files/FZJ-22984.jpg?subformat=icon-640
|x icon-640
|y OpenAccess
909 C O |o oai:juser.fz-juelich.de:22984
|p openaire
|p open_access
|p driver
|p VDB
|p dnbdelivery
913 1 _ |0 G:(DE-Juel1)FUEK491
|1 G:(DE-HGF)POF2-230
|2 G:(DE-HGF)POF2-200
|a DE-HGF
|b Erde und Umwelt
|k P23
|l Atmosphäre und Klima
|v Atmosphäre und Klima
|x 0
|z vormals P22
913 2 _ |0 G:(DE-HGF)POF3-582
|1 G:(DE-HGF)POF3-580
|2 G:(DE-HGF)POF3-500
|a DE-HGF
|b Key Technologies
|l Key Technologies for the Bioeconomy
|v Plant Science
|x 0
914 1 _ |y 2012
915 _ _ |0 LIC:(DE-HGF)CCBY3
|2 HGFVOC
|a Creative Commons Attribution CC BY 3.0
915 _ _ |0 StatID:(DE-HGF)0010
|2 StatID
|a JCR/ISI refereed
915 _ _ |0 StatID:(DE-HGF)0100
|2 StatID
|a JCR
915 _ _ |0 StatID:(DE-HGF)0110
|2 StatID
|a WoS
|b Science Citation Index
915 _ _ |0 StatID:(DE-HGF)0111
|2 StatID
|a WoS
|b Science Citation Index Expanded
915 _ _ |0 StatID:(DE-HGF)0150
|2 StatID
|a DBCoverage
|b Web of Science Core Collection
915 _ _ |0 StatID:(DE-HGF)0199
|2 StatID
|a DBCoverage
|b Thomson Reuters Master Journal List
915 _ _ |0 StatID:(DE-HGF)0200
|2 StatID
|a DBCoverage
|b SCOPUS
915 _ _ |0 StatID:(DE-HGF)0300
|2 StatID
|a DBCoverage
|b Medline
915 _ _ |0 StatID:(DE-HGF)0500
|2 StatID
|a DBCoverage
|b DOAJ
915 _ _ |0 StatID:(DE-HGF)0510
|2 StatID
|a OpenAccess
915 _ _ |0 StatID:(DE-HGF)1020
|2 StatID
|a DBCoverage
|b Current Contents - Social and Behavioral Sciences
920 1 _ |0 I:(DE-Juel1)IEK-8-20101013
|g IEK
|k IEK-8
|l Troposphäre
|x 0
920 1 _ |0 I:(DE-Juel1)IBG-2-20101118
|g IBG
|k IBG-2
|l Pflanzenwissenschaften
|x 1
970 _ _ |a VDB:(DE-Juel1)139849
980 1 _ |a FullTexts
980 _ _ |a VDB
980 _ _ |a ConvertedRecord
980 _ _ |a journal
980 _ _ |a I:(DE-Juel1)IEK-8-20101013
980 _ _ |a I:(DE-Juel1)IBG-2-20101118
980 _ _ |a UNRESTRICTED
980 _ _ |a JUWEL
980 _ _ |a FullTexts
981 _ _ |a I:(DE-Juel1)ICE-3-20101013
981 _ _ |a I:(DE-Juel1)IBG-2-20101118


LibraryCollectionCLSMajorCLSMinorLanguageAuthor
Marc 21