Ground-based aerosol characterization during the South American Biomass Burning Analysis (SAMBBA) field experiment

Detalhes bibliográficos
Autor(a) principal: Brito, Joel Ferreira
Data de Publicação: 2014
Outros Autores: Rizzo, Luciana Varanda [UNIFESP], Morgan, Willian T., Coe, Hugh, Johnson, Ben, Haywood, Jim, Longo, Karla Maria, Freitas, Saulo, Andreae, Meinrat O., Artaxo, Paulo
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UNIFESP
Texto Completo: http://dx.doi.org/10.5194/acp-14-12069-2014
http://repositorio.unifesp.br/handle/11600/37194
Resumo: This paper investigates the physical and chemical characteristics of aerosols at ground level at a site heavily impacted by biomass burning. the site is located near Porto Velho, Rondonia, in the southwestern part of the Brazilian Amazon rainforest, and was selected for the deployment of a large suite of instruments, among them an Aerosol Chemical Speciation Monitor. Our measurements were made during the South American Biomass Burning Analysis (SAMBBA) field experiment, which consisted of a combination of aircraft and ground-based measurements over Brazil, aimed to investigate the impacts of biomass burning emissions on climate, air quality, and numerical weather prediction over South America. the campaign took place during the dry season and the transition to the wet season in September/October 2012.During most of the campaign, the site was impacted by regional biomass burning pollution (average CO mixing ratio of 0.6 ppm), occasionally superimposed by intense (up to 2 ppm of CO), freshly emitted biomass burning plumes. Aerosol number concentrations ranged from similar to 1000 cm(-3) to peaks of up to 35 000 cm(-3) (during biomass burning (BB) events, corresponding to an average submicron mass mean concentrations of 13.7 mu g m(-3) and peak concentrations close to 100 mu g m-3. Organic aerosol strongly dominated the submicron non-refractory composition, with an average concen-tration of 11.4 mu g m(-3). the inorganic species, NH4, SO4, NO3, and Cl, were observed, on average, at concentrations of 0.44, 0.34, 0.19, and 0.01 mu g m(-3), respectively. Equivalent black carbon (BCe) ranged from 0.2 to 5.5 mu g m(-3), with an average concentration of 1.3 mu g m(-3). During BB peaks, organics accounted for over 90% of total mass (submicron non-refractory plus BCe), among the highest values described in the literature.We examined the ageing of biomass burning organic aerosol (BBOA) using the changes in the H : C and O : C ratios, and found that throughout most of the aerosol processing (O : C congruent to D 0 : 25 to O : C congruent to D 0 : 6), no remarkable change is observed in the H : C ratio (similar to 1 : 35). Such a result contrasts strongly with previous observations of chemical ageing of both urban and Amazonian biogenic aerosols. At higher levels of processing (O : C > 0 : 6), the H : C ratio changes with a H : C / O : C slope of -0.5, possibly due to the development of a combination of BB (H : C / O : C slope D 0) and biogenic (H : C / O : C slope D 1) organic aerosol (OA). An analysis of the Delta OA / Delta CO mass ratios yields very little enhancement in the OA loading with atmospheric processing, consistent with previous observations. These results indicate that negligible secondary organic aerosol (SOA) formation occurs throughout the observed BB plume processing, or that SOA formation is almost entirely balanced by OA volatilization.Positive matrix factorization (PMF) of the organic aerosol spectra resulted in three factors: fresh BBOA, aged BBOA, and low-volatility oxygenated organic aerosol (LV-OOA). Analysis of the diurnal patterns and correlation with external markers indicates that during the first part of the campaign, OA concentrations are impacted by local fire plumes with some chemical processing occurring in the near-surface layer. During the second part of the campaign, long-range transport of BB plumes above the surface layer, as well as potential SOAs formed aloft, dominates OA concentrations at our ground-based sampling site.This manuscript describes the first ground-based deployment of the aerosol mass spectrometry at a site heavily impacted by biomass burning in the Amazon region, allowing a deeper understanding of aerosol life cycle in this important ecosystem.
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spelling Ground-based aerosol characterization during the South American Biomass Burning Analysis (SAMBBA) field experimentThis paper investigates the physical and chemical characteristics of aerosols at ground level at a site heavily impacted by biomass burning. the site is located near Porto Velho, Rondonia, in the southwestern part of the Brazilian Amazon rainforest, and was selected for the deployment of a large suite of instruments, among them an Aerosol Chemical Speciation Monitor. Our measurements were made during the South American Biomass Burning Analysis (SAMBBA) field experiment, which consisted of a combination of aircraft and ground-based measurements over Brazil, aimed to investigate the impacts of biomass burning emissions on climate, air quality, and numerical weather prediction over South America. the campaign took place during the dry season and the transition to the wet season in September/October 2012.During most of the campaign, the site was impacted by regional biomass burning pollution (average CO mixing ratio of 0.6 ppm), occasionally superimposed by intense (up to 2 ppm of CO), freshly emitted biomass burning plumes. Aerosol number concentrations ranged from similar to 1000 cm(-3) to peaks of up to 35 000 cm(-3) (during biomass burning (BB) events, corresponding to an average submicron mass mean concentrations of 13.7 mu g m(-3) and peak concentrations close to 100 mu g m-3. Organic aerosol strongly dominated the submicron non-refractory composition, with an average concen-tration of 11.4 mu g m(-3). the inorganic species, NH4, SO4, NO3, and Cl, were observed, on average, at concentrations of 0.44, 0.34, 0.19, and 0.01 mu g m(-3), respectively. Equivalent black carbon (BCe) ranged from 0.2 to 5.5 mu g m(-3), with an average concentration of 1.3 mu g m(-3). During BB peaks, organics accounted for over 90% of total mass (submicron non-refractory plus BCe), among the highest values described in the literature.We examined the ageing of biomass burning organic aerosol (BBOA) using the changes in the H : C and O : C ratios, and found that throughout most of the aerosol processing (O : C congruent to D 0 : 25 to O : C congruent to D 0 : 6), no remarkable change is observed in the H : C ratio (similar to 1 : 35). Such a result contrasts strongly with previous observations of chemical ageing of both urban and Amazonian biogenic aerosols. At higher levels of processing (O : C > 0 : 6), the H : C ratio changes with a H : C / O : C slope of -0.5, possibly due to the development of a combination of BB (H : C / O : C slope D 0) and biogenic (H : C / O : C slope D 1) organic aerosol (OA). An analysis of the Delta OA / Delta CO mass ratios yields very little enhancement in the OA loading with atmospheric processing, consistent with previous observations. These results indicate that negligible secondary organic aerosol (SOA) formation occurs throughout the observed BB plume processing, or that SOA formation is almost entirely balanced by OA volatilization.Positive matrix factorization (PMF) of the organic aerosol spectra resulted in three factors: fresh BBOA, aged BBOA, and low-volatility oxygenated organic aerosol (LV-OOA). Analysis of the diurnal patterns and correlation with external markers indicates that during the first part of the campaign, OA concentrations are impacted by local fire plumes with some chemical processing occurring in the near-surface layer. During the second part of the campaign, long-range transport of BB plumes above the surface layer, as well as potential SOAs formed aloft, dominates OA concentrations at our ground-based sampling site.This manuscript describes the first ground-based deployment of the aerosol mass spectrometry at a site heavily impacted by biomass burning in the Amazon region, allowing a deeper understanding of aerosol life cycle in this important ecosystem.Univ São Paulo, Inst Phys, São Paulo, BrazilUniversidade Federal de São Paulo, Dept Earth & Exact Sci, Diadema, BrazilUniv Manchester, Sch Earth Atmospher & Environm Sci, Ctr Atmospher Sci, Manchester, Lancs, EnglandUK Met Off, Exeter, Devon, EnglandUniv Exeter, Coll Engn Maths & Phys Sci, Exeter, Devon, EnglandNatl Inst Space Res INPE, Sao Jose Dos Campos, BrazilMax Planck Inst Chem, Biogeochem Dept, D-55128 Mainz, GermanyUniversidade Federal de São Paulo, Dept Earth & Exact Sci, Diadema, BrazilWeb of ScienceFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)INCT AmazoniaNatural Environment Research Council (NERC)FAPESP: 2012/14437-9FAPESP: 2013/05014-0CNPq: 475735-2012-9Natural Environment Research Council (NERC): NE/J010073/1Copernicus Gesellschaft MbhUniversidade de São Paulo (USP)Universidade Federal de São Paulo (UNIFESP)Univ ManchesterUK Met OffUniv ExeterNatl Inst Space Res INPEMax Planck Inst ChemBrito, Joel FerreiraRizzo, Luciana Varanda [UNIFESP]Morgan, Willian T.Coe, HughJohnson, BenHaywood, JimLongo, Karla MariaFreitas, SauloAndreae, Meinrat O.Artaxo, Paulo2016-01-24T14:35:00Z2016-01-24T14:35:00Z2014-01-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersion12069-12083application/pdfhttp://dx.doi.org/10.5194/acp-14-12069-2014Atmospheric Chemistry and Physics. Gottingen: Copernicus Gesellschaft Mbh, v. 14, n. 22, p. 12069-12083, 2014.10.5194/acp-14-12069-2014WOS000345290700004.pdf1680-7316http://repositorio.unifesp.br/handle/11600/37194WOS:000345290700004engAtmospheric Chemistry and Physicsinfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da UNIFESPinstname:Universidade Federal de São Paulo (UNIFESP)instacron:UNIFESP2024-07-31T17:34:36Zoai:repositorio.unifesp.br/:11600/37194Repositório InstitucionalPUBhttp://www.repositorio.unifesp.br/oai/requestbiblioteca.csp@unifesp.bropendoar:34652024-07-31T17:34:36Repositório Institucional da UNIFESP - Universidade Federal de São Paulo (UNIFESP)false
dc.title.none.fl_str_mv Ground-based aerosol characterization during the South American Biomass Burning Analysis (SAMBBA) field experiment
title Ground-based aerosol characterization during the South American Biomass Burning Analysis (SAMBBA) field experiment
spellingShingle Ground-based aerosol characterization during the South American Biomass Burning Analysis (SAMBBA) field experiment
Brito, Joel Ferreira
title_short Ground-based aerosol characterization during the South American Biomass Burning Analysis (SAMBBA) field experiment
title_full Ground-based aerosol characterization during the South American Biomass Burning Analysis (SAMBBA) field experiment
title_fullStr Ground-based aerosol characterization during the South American Biomass Burning Analysis (SAMBBA) field experiment
title_full_unstemmed Ground-based aerosol characterization during the South American Biomass Burning Analysis (SAMBBA) field experiment
title_sort Ground-based aerosol characterization during the South American Biomass Burning Analysis (SAMBBA) field experiment
author Brito, Joel Ferreira
author_facet Brito, Joel Ferreira
Rizzo, Luciana Varanda [UNIFESP]
Morgan, Willian T.
Coe, Hugh
Johnson, Ben
Haywood, Jim
Longo, Karla Maria
Freitas, Saulo
Andreae, Meinrat O.
Artaxo, Paulo
author_role author
author2 Rizzo, Luciana Varanda [UNIFESP]
Morgan, Willian T.
Coe, Hugh
Johnson, Ben
Haywood, Jim
Longo, Karla Maria
Freitas, Saulo
Andreae, Meinrat O.
Artaxo, Paulo
author2_role author
author
author
author
author
author
author
author
author
dc.contributor.none.fl_str_mv Universidade de São Paulo (USP)
Universidade Federal de São Paulo (UNIFESP)
Univ Manchester
UK Met Off
Univ Exeter
Natl Inst Space Res INPE
Max Planck Inst Chem
dc.contributor.author.fl_str_mv Brito, Joel Ferreira
Rizzo, Luciana Varanda [UNIFESP]
Morgan, Willian T.
Coe, Hugh
Johnson, Ben
Haywood, Jim
Longo, Karla Maria
Freitas, Saulo
Andreae, Meinrat O.
Artaxo, Paulo
description This paper investigates the physical and chemical characteristics of aerosols at ground level at a site heavily impacted by biomass burning. the site is located near Porto Velho, Rondonia, in the southwestern part of the Brazilian Amazon rainforest, and was selected for the deployment of a large suite of instruments, among them an Aerosol Chemical Speciation Monitor. Our measurements were made during the South American Biomass Burning Analysis (SAMBBA) field experiment, which consisted of a combination of aircraft and ground-based measurements over Brazil, aimed to investigate the impacts of biomass burning emissions on climate, air quality, and numerical weather prediction over South America. the campaign took place during the dry season and the transition to the wet season in September/October 2012.During most of the campaign, the site was impacted by regional biomass burning pollution (average CO mixing ratio of 0.6 ppm), occasionally superimposed by intense (up to 2 ppm of CO), freshly emitted biomass burning plumes. Aerosol number concentrations ranged from similar to 1000 cm(-3) to peaks of up to 35 000 cm(-3) (during biomass burning (BB) events, corresponding to an average submicron mass mean concentrations of 13.7 mu g m(-3) and peak concentrations close to 100 mu g m-3. Organic aerosol strongly dominated the submicron non-refractory composition, with an average concen-tration of 11.4 mu g m(-3). the inorganic species, NH4, SO4, NO3, and Cl, were observed, on average, at concentrations of 0.44, 0.34, 0.19, and 0.01 mu g m(-3), respectively. Equivalent black carbon (BCe) ranged from 0.2 to 5.5 mu g m(-3), with an average concentration of 1.3 mu g m(-3). During BB peaks, organics accounted for over 90% of total mass (submicron non-refractory plus BCe), among the highest values described in the literature.We examined the ageing of biomass burning organic aerosol (BBOA) using the changes in the H : C and O : C ratios, and found that throughout most of the aerosol processing (O : C congruent to D 0 : 25 to O : C congruent to D 0 : 6), no remarkable change is observed in the H : C ratio (similar to 1 : 35). Such a result contrasts strongly with previous observations of chemical ageing of both urban and Amazonian biogenic aerosols. At higher levels of processing (O : C > 0 : 6), the H : C ratio changes with a H : C / O : C slope of -0.5, possibly due to the development of a combination of BB (H : C / O : C slope D 0) and biogenic (H : C / O : C slope D 1) organic aerosol (OA). An analysis of the Delta OA / Delta CO mass ratios yields very little enhancement in the OA loading with atmospheric processing, consistent with previous observations. These results indicate that negligible secondary organic aerosol (SOA) formation occurs throughout the observed BB plume processing, or that SOA formation is almost entirely balanced by OA volatilization.Positive matrix factorization (PMF) of the organic aerosol spectra resulted in three factors: fresh BBOA, aged BBOA, and low-volatility oxygenated organic aerosol (LV-OOA). Analysis of the diurnal patterns and correlation with external markers indicates that during the first part of the campaign, OA concentrations are impacted by local fire plumes with some chemical processing occurring in the near-surface layer. During the second part of the campaign, long-range transport of BB plumes above the surface layer, as well as potential SOAs formed aloft, dominates OA concentrations at our ground-based sampling site.This manuscript describes the first ground-based deployment of the aerosol mass spectrometry at a site heavily impacted by biomass burning in the Amazon region, allowing a deeper understanding of aerosol life cycle in this important ecosystem.
publishDate 2014
dc.date.none.fl_str_mv 2014-01-01
2016-01-24T14:35:00Z
2016-01-24T14:35:00Z
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://dx.doi.org/10.5194/acp-14-12069-2014
Atmospheric Chemistry and Physics. Gottingen: Copernicus Gesellschaft Mbh, v. 14, n. 22, p. 12069-12083, 2014.
10.5194/acp-14-12069-2014
WOS000345290700004.pdf
1680-7316
http://repositorio.unifesp.br/handle/11600/37194
WOS:000345290700004
url http://dx.doi.org/10.5194/acp-14-12069-2014
http://repositorio.unifesp.br/handle/11600/37194
identifier_str_mv Atmospheric Chemistry and Physics. Gottingen: Copernicus Gesellschaft Mbh, v. 14, n. 22, p. 12069-12083, 2014.
10.5194/acp-14-12069-2014
WOS000345290700004.pdf
1680-7316
WOS:000345290700004
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv Atmospheric Chemistry and Physics
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv 12069-12083
application/pdf
dc.publisher.none.fl_str_mv Copernicus Gesellschaft Mbh
publisher.none.fl_str_mv Copernicus Gesellschaft Mbh
dc.source.none.fl_str_mv reponame:Repositório Institucional da UNIFESP
instname:Universidade Federal de São Paulo (UNIFESP)
instacron:UNIFESP
instname_str Universidade Federal de São Paulo (UNIFESP)
instacron_str UNIFESP
institution UNIFESP
reponame_str Repositório Institucional da UNIFESP
collection Repositório Institucional da UNIFESP
repository.name.fl_str_mv Repositório Institucional da UNIFESP - Universidade Federal de São Paulo (UNIFESP)
repository.mail.fl_str_mv biblioteca.csp@unifesp.br
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