An analysis of diurnal cycles in the mass of ambient aerosols derived from biomass burning and agro-industry

dc.contributor.authorCaetano-Silva, L. [UNESP]
dc.contributor.authorAllen, A. G. [UNESP]
dc.contributor.authorLima-Souza, M. [UNESP]
dc.contributor.authorCardoso, Arnaldo Alves [UNESP]
dc.contributor.authorCampos, M. L A M
dc.contributor.authorNogueira, Raquel Fernandes Pupo [UNESP]
dc.contributor.institutionUniversidade Estadual Paulista (Unesp)
dc.contributor.institutionUniversidade de São Paulo (USP)
dc.date.accessioned2014-05-27T11:30:09Z
dc.date.available2014-05-27T11:30:09Z
dc.date.issued2013-08-16
dc.description.abstractStrong diurnal cycles in ambient aerosol mass were observed in a rural region of Southeast Brazil where the trace composition of the lower troposphere is governed mainly by emissions from agro-industry. An optical particle counter was used to record size-segregated aerosol number concentrations between 13 May 2010 and 15 March 2011. The data were collected every 10 min and used to calculate aerosol mass concentrations. Aerosol samples were also collected onto filters during daytime (10:00-16:00 local time) and nighttime (20:00-06:00) periods, for subsequent analysis of soluble ions and water-soluble organic carbon. Biomass burning aerosols predominated during the dry winter, while secondary aerosols were most important in the summer rainy season. In both seasons, diurnal cycles in calculated aerosol mass concentrations were due to the uptake of water by the aerosols and, to a lesser extent, to emissions and secondary aerosol formation. In neither season could the observed mass changes be explained by changes in the depth of the boundary layer. In the summer, nighttime increases in aerosol mass ranged from 2.7-fold to 81-fold, depending on particle size, while in the winter, the range was narrower, from 2.2-fold to 9.5-fold, supporting the possibility that the presence of particles derived from biomass burning reduced the overall ability of the aerosols to absorb water. Key Points Diurnal cycle of agro-industrial aerosol mass governed by humidity Biomass burning emissions act to suppress particle growth Need to consider diurnal mass cycles in aerosol dry deposition models ©2013. American Geophysical Union. All Rights Reserved.en
dc.description.affiliationInstituto de Química Universidade Estadual Paulista, 14801-970, Araraquara, São Paulo
dc.description.affiliationDepartamento de Química Faculdade de Filosofia, Ciências e Letras de Ribeirão Preto Universidade de São Paulo, Ribeirão Preto
dc.description.affiliationUnespInstituto de Química Universidade Estadual Paulista, 14801-970, Araraquara, São Paulo
dc.format.extent8675-8687
dc.identifierhttp://dx.doi.org/10.1002/jgrd.50630
dc.identifier.citationJournal of Geophysical Research D: Atmospheres, v. 118, n. 15, p. 8675-8687, 2013.
dc.identifier.doi10.1002/jgrd.50630
dc.identifier.issn0148-0227
dc.identifier.issn2169-8996
dc.identifier.lattes9165109840414837
dc.identifier.lattes6887310539435086
dc.identifier.orcid0000-0003-1237-4571
dc.identifier.scopus2-s2.0-84884163164
dc.identifier.urihttp://hdl.handle.net/11449/76278
dc.identifier.wosWOS:000324032900039
dc.language.isoeng
dc.relation.ispartofJournal of Geophysical Research D: Atmospheres
dc.relation.ispartofsjr1,823
dc.rights.accessRightsAcesso restrito
dc.sourceScopus
dc.subjectaerosols
dc.subjectagro-industry
dc.subjectbiomass burning
dc.subjectdiurnal cycle
dc.subjecthygroscopicity
dc.subjectmass
dc.titleAn analysis of diurnal cycles in the mass of ambient aerosols derived from biomass burning and agro-industryen
dc.typeArtigo
dcterms.licensehttp://olabout.wiley.com/WileyCDA/Section/id-406071.html
unesp.author.lattes9165109840414837[4]
unesp.author.lattes6887310539435086[6]
unesp.author.orcid0000-0003-2046-995X[4]
unesp.author.orcid0000-0003-1237-4571[6]
unesp.campusUniversidade Estadual Paulista (Unesp), Instituto de Química, Araraquarapt

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