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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21c.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34R/3R44Q9H
Repositóriosid.inpe.br/mtc-m21c/2018/05.08.17.04
Última Atualização2018:05.08.17.04.11 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m21c/2018/05.08.17.04.11
Última Atualização dos Metadados2022:03.05.04.09.20 (UTC) administrator
DOI10.5194/acp-2018-232
ISSN1680-7367
Chave de CitaçãoSchulzSHACSDFJKKMMPSVWZZAAMPWB:2018:AiObIs
TítuloAircraft-based observations of isoprene epoxydiol-derived secondary organic aerosol (IEPOX-SOA) in the tropical upper troposphere over the Amazon region
Ano2018
Data de Acesso02 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho825 KiB
2. Contextualização
Autor 1 Schulz, Christiane
 2 Schneider, Johannes
 3 Holanda, Bruna Amorim
 4 Appel, Oliver
 5 Costa, Anja
 6 Sá, Suzane S. de
 7 Dreiling, Volker
 8 Fütterer, Daniel
 9 Jurkat-Witschas, Tina
10 Klimach, Thomas
11 Krämer, Martina
12 Martin, Scot T.
13 Mertes, Stephan
14 Pöhlker, Mira L.
15 Sauer, Daniel
16 Voigt, Christiane
17 Weinzierl, Bernadett
18 Ziereis, Helmut
19 Zöger, Martin
20 Andreae, Meinrat O.
21 Artaxo, Paulo
22 Machado, Luiz Augusto Toledo
23 Pöschl, Ulrich
24 Wendisch, Manfred
25 Borrmann, Stephan
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Afiliação 1 Max Planck Institute for Chemistry
 2 Max Planck Institute for Chemistry
 3 Max Planck Institute for Chemistry
 4 Max Planck Institute for Chemistry
 5 Institut für Energie- und Klimaforschung (IEK7)
 6 Harvard University
 7 German Aerospace Center (Deutsches Zentrum für Luft- und Raumfahrt)
 8 German Aerospace Center (Deutsches Zentrum für Luft- und Raumfahrt)
 9 German Aerospace Center (Deutsches Zentrum für Luft- und Raumfahrt)
10 Max Planck Institute for Chemistry
11 Institut für Energie- und Klimaforschung (IEK7)
12 Harvard University
13 Leibniz Institute for Tropospheric Research
14 Max Planck Institute for Chemistry
15 German Aerospace Center (Deutsches Zentrum für Luft- und Raumfahrt)
16 German Aerospace Center (Deutsches Zentrum für Luft- und Raumfahrt)
17 German Aerospace Center (Deutsches Zentrum für Luft- und Raumfahrt)
18 German Aerospace Center (Deutsches Zentrum für Luft- und Raumfahrt)
19 German Aerospace Center (Deutsches Zentrum für Luft- und Raumfahrt)
20 Max Planck Institute for Chemistry
21 Universidade de São Paulo (USP)
22 Instituto Nacional de Pesquisas Espaciais (INPE)
23 Max Planck Institute for Chemistry
24 University of Leipzig
25 Max Planck Institute for Chemistry
Endereço de e-Mail do Autor 1
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RevistaAtmospheric Chemistry and Physics Discussion
Volume2018
Número232
Nota SecundáriaC_ASTRONOMIA_/_FÍSICA
Histórico (UTC)2018-05-08 17:04:11 :: simone -> administrator ::
2018-05-08 17:04:11 :: administrator -> simone :: 2018
2018-05-08 17:09:38 :: simone -> administrator :: 2018
2022-03-05 04:09:20 :: administrator -> simone :: 2018
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
ResumoDuring the ACRIDICON-CHUVA field project (SeptemberOctober 2014; based in Manaus, Brazil) aircraft-based in-situ measurements of aerosol chemical composition were conducted in the tropical troposphere over the Amazon using the High Altitude and Long Range Research Aircraft (HALO), covering altitudes from the boundary layer height up to 14.4 km. The submicron non-refractory aerosol was characterized by flash-vaporization/electron impact-ionization aerosol particle mass spectrometry. The results show that significant secondary organic aerosol (SOA) formation by isoprene oxidation products occurs in the upper troposphere, leading to increased organic aerosol mass concentrations above 10 km altitude. The median organic mass concentrations in the upper troposphere above 10 km range between 1.0 and 2.1 μg m−3 (referring to standard temperature and pressure; STP) with interquartile ranges of 0.6 to 3.0 μg m−3 (STP), representing 70 % of the total submicron non-refractory aerosol particle mass. The presence of isoprene epoxydiol-derived isoprene secondary organic aerosol (IEPOX-SOA) was confirmed by marker peaks in the mass spectra. We estimate the contribution of IEPOX-SOA to the total organic aerosol in the upper troposphere to be about 20 %. After isoprene emission from vegetation, oxidation processes occur at low altitudes and/or during transport to higher altitudes, which may lead to the formation of IEPOX (one oxidation product of isoprene). Reactive uptake or condensation of IEPOX on pre-existing particles leads to IEPOX-SOA formation and subsequently increasing organic mass in the upper troposphere. This organic mass increase was accompanied by an increase of the nitrate mass concentrations, most likely due to NOx production by lightning. We further found that the ammonium contained in the aerosol particles is not sufficient to neutralize the particulate sulfate and nitrate. Analysis of the ion ratio of NO+ to NO2+ indicated that nitrate in the upper troposphere exists mainly in the form of organic nitrate. IEPOX-SOA and organic nitrates are coincident with each other, indicating that IEPOX-SOA forms in the upper troposphere either on acidic nitrate particles forming organic nitrates derived from IEPOX or on already neutralized organic nitrate aerosol particles.
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4. Condições de acesso e uso
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Arquivo Alvoschulz_aircraft.pdf
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5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/43SRC6S
Lista de Itens Citandosid.inpe.br/bibdigital/2021/01.03.02.10 2
DivulgaçãoWEBSCI; PORTALCAPES.
Acervo Hospedeirourlib.net/www/2017/11.22.19.04
6. Notas
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