001     6233
005     20240712100946.0
024 7 _ |2 pmid
|a pmid:19924939
024 7 _ |2 DOI
|a 10.1021/es901420b
024 7 _ |2 WOS
|a WOS:000271106300033
024 7 _ |2 ISSN
|a 0013-936X
024 7 _ |2 ISSN
|a 1520-5851
037 _ _ |a PreJuSER-6233
041 _ _ |a eng
082 _ _ |a 050
084 _ _ |2 WoS
|a Engineering, Environmental
084 _ _ |2 WoS
|a Environmental Sciences
100 1 _ |0 P:(DE-Juel1)4528
|a Kiendler-Scharr, A.
|b 0
|u FZJ
245 _ _ |a Aerosol Mass Spectrometric Features of Biogenic SOA: Observations from a Plant Chamber and in Rural Atmospheric Environments
260 _ _ |a Columbus, Ohio
|b American Chemical Society
|c 2009
300 _ _ |a 8166 - 8172
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 1865
|a Environmental Science and Technology
|v 43
|x 0013-936X
|y 21
500 _ _ |a We gratefully acknowledge support by the European Commission (IP-EUCAARI, Contract No. 036833-2). Q.Z. was supported by the U.S. Department of Energy's Atmospheric Science Program (Office of Science, BER), Grant No. DE-FG02-08ER64627. We thank James Allan (U. Manchester) for the AMS data analysis software and anonymous reviewers for their constructive comments.
520 _ _ |a Secondary organic aerosol (SOA) is known to form from a variety of anthropogenic and biogenic precursors. Current estimates of global SOA production vary over 2 orders of magnitude. Since no direct measurement technique for SOA exists, quantifying SOA remains a challenge for atmospheric studies. The identification of biogenic SOA (BSOA) based on mass spectral signatures offers the possibility to derive source information of organic aerosol (OA) with high time resolution. Here we present data from simulation experiments. The BSOA from tree emissions was characterized with an Aerodyne quadrupole aerosol mass spectrometer (Q-AMS). Collection efficiencies were close to 1, and effective densities of the BSOA were found to be 1.3 +/- 0.1 g/cm(3). The mass spectra of SOA from different trees were found to be highly similar. The average BSOA mass spectrum from tree emissions is compared to a BSOA component spectrum extracted from field data. It is shown that overall the spectra agree well and that the mass spectral features of BSOA are distinctively different from those of OA components related to fresh fossil fuel and biomass combustions. The simulation chamber mass spectrum may potentially be useful for the identification and interpretation of biogenic SOA components in ambient data sets.
536 _ _ |0 G:(DE-Juel1)FUEK406
|2 G:(DE-HGF)
|a Atmosphäre und Klima
|c P22
|x 0
536 _ _ |0 G:(DE-Juel1)FUEK407
|2 G:(DE-HGF)
|a Terrestrische Umwelt
|c P24
|x 1
588 _ _ |a Dataset connected to Web of Science, Pubmed
650 _ 2 |2 MeSH
|a Aerosols: analysis
650 _ 2 |2 MeSH
|a Atmosphere: chemistry
650 _ 2 |2 MeSH
|a Mass Spectrometry
650 _ 2 |2 MeSH
|a Organic Chemicals: analysis
650 _ 2 |2 MeSH
|a Particle Size
650 _ 2 |2 MeSH
|a Time Factors
650 _ 2 |2 MeSH
|a Trees: chemistry
650 _ 2 |2 MeSH
|a Volatilization
650 _ 7 |0 0
|2 NLM Chemicals
|a Aerosols
650 _ 7 |0 0
|2 NLM Chemicals
|a Organic Chemicals
650 _ 7 |2 WoSType
|a J
700 1 _ |0 P:(DE-HGF)0
|a Zhang, Q.
|b 1
700 1 _ |0 P:(DE-Juel1)VDB72897
|a Hohaus, Th.
|b 2
|u FZJ
700 1 _ |0 P:(DE-Juel1)129345
|a Kleist, E.
|b 3
|u FZJ
700 1 _ |0 P:(DE-Juel1)VDB66036
|a Mensah, A.
|b 4
|u FZJ
700 1 _ |0 P:(DE-Juel1)16346
|a Mentel, T. F.
|b 5
|u FZJ
700 1 _ |0 P:(DE-Juel1)VDB73341
|a Spindler, C.
|b 6
|u FZJ
700 1 _ |0 P:(DE-Juel1)VDB56253
|a Uerlings, R.
|b 7
|u FZJ
700 1 _ |0 P:(DE-Juel1)5344
|a Tillmann, R.
|b 8
|u FZJ
700 1 _ |0 P:(DE-Juel1)VDB1780
|a Wildt, J.
|b 9
|u FZJ
773 _ _ |0 PERI:(DE-600)1465132-4
|a 10.1021/es901420b
|g Vol. 43, p. 8166 - 8172
|p 8166 - 8172
|q 43<8166 - 8172
|t Environmental Science & Technology
|v 43
|x 0013-936X
|y 2009
856 7 _ |u http://dx.doi.org/10.1021/es901420b
856 4 _ |u https://juser.fz-juelich.de/record/6233/files/FZJ-6233.pdf
|z Published final document.
|y Restricted
909 C O |o oai:juser.fz-juelich.de:6233
|p VDB
913 1 _ |0 G:(DE-Juel1)FUEK406
|a DE-HGF
|b Umwelt
|k P22
|l Atmosphäre und Klima
|v Atmosphäre und Klima
|x 0
|z fortgesetzt als P23
913 1 _ |0 G:(DE-Juel1)FUEK407
|a DE-HGF
|b Erde und Umwelt
|k P24
|l Terrestrische Umwelt
|v Terrestrische Umwelt
|x 1
914 1 _ |y 2009
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)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)0300
|2 StatID
|a DBCoverage
|b Medline
920 1 _ |0 I:(DE-Juel1)VDB791
|d 30.09.2010
|g ICG
|k ICG-2
|l Troposphäre
|x 1
920 1 _ |0 I:(DE-Juel1)ICG-3-20090406
|d 31.10.2010
|g ICG
|k ICG-3
|l Phytosphäre
|x 2
970 _ _ |a VDB:(DE-Juel1)114388
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
981 _ _ |a I:(DE-Juel1)ICE-3-20101013
981 _ _ |a I:(DE-Juel1)IEK-8-20101013
981 _ _ |a I:(DE-Juel1)IBG-2-20101118
981 _ _ |a I:(DE-Juel1)ICG-3-20090406


LibraryCollectionCLSMajorCLSMinorLanguageAuthor
Marc 21