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Log smoldering after an Amazonian deforestation fire

dc.contributor.authorRabelo, ERC
dc.contributor.authorVeras, CAG
dc.contributor.authorCarvalho, J. A.
dc.contributor.authorAlvarado, E. C.
dc.contributor.authorSandberg, D. V.
dc.contributor.authorSantos, J. C.
dc.contributor.institutionUniversidade Estadual Paulista (Unesp)
dc.contributor.institutionUniversidade de Brasília (UnB)
dc.contributor.institutionUniversity of Washington
dc.contributor.institutionUS Forest Serv
dc.contributor.institutionInstituto Nacional de Pesquisas Espaciais (INPE)
dc.date.accessioned2014-05-20T13:27:27Z
dc.date.available2014-05-20T13:27:27Z
dc.date.issued2004-01-01
dc.description.abstractThe characteristics of log smoldering after an Amazonian deforestation fire are described. The experiment was carried out in 2001 at the Caiabi farm, near the city of Alta Floresta, state of Mato Grosso, Brazil, as part of a set of tests that have been performed in the same area since 1997. A 200 x 200m(2) test area was slashed in the beginning of June and burned on 20 August. The area contained 507 logs with diameter at breast height (DBH) higher than 10 cm, per hectare. In the day following the main burn 59 logs were found to remain smoldering, a number that corresponds to 2.9% of the total in the area. We chose 11 of the 59 logs to have their smoldering process monitored. Their diameter, moisture content and CHN dry biomass composition after the plot burn and before smoldering were determined. Other parameters such as temperature distribution while smoldering, porosity, density and mass volatilized during thermogravimetric test were also determined. Average smoldering speeds were in the range from 0.8 to 1.5 cm h(-1) for logs that smoldered without transition to the flaming regime. The average speed increased to 2.1 cm h(-1) for those logs that oscillated between smoldering and flaming. The speeds were lower overnight as compared to values determined during daytime for the same log. Higher log moisture contents were found to produce decreased speeds. Micro-porous biomass was not observed in the set of the 11 selected logs. Smoldering was observed to occur at substantial intensity in crossing of logs, with no longitudinal propagation. (C) 2003 Elsevier Ltd. All rights reserved.en
dc.description.affiliationUniv Estadual Paulista, UNESP, Dept Energia, BR-12516410 Guaratingueta, SP, Brazil
dc.description.affiliationUniv Brasilia, UnB, BR-70910900 Brasilia, DF, Brazil
dc.description.affiliationUniv Washington, Coll Forest Resources, Seattle, WA 98195 USA
dc.description.affiliationUS Forest Serv, USDA, Corvallis, OR 97331 USA
dc.description.affiliationInst Nacl Pesquisas Espaciais, BR-12630000 Cachoeira Paulista, SP, Brazil
dc.description.affiliationUnespUniv Estadual Paulista, UNESP, Dept Energia, BR-12516410 Guaratingueta, SP, Brazil
dc.format.extent203-211
dc.identifierhttp://dx.doi.org/10.1016/j.atmosenv.2003.09.065
dc.identifier.citationAtmospheric Environment. Oxford: Pergamon-Elsevier B.V., v. 38, n. 2, p. 203-211, 2004.
dc.identifier.doi10.1016/j.atmosenv.2003.09.065
dc.identifier.issn1352-2310
dc.identifier.urihttp://hdl.handle.net/11449/9028
dc.identifier.wosWOS:000188210700004
dc.language.isoeng
dc.publisherElsevier B.V.
dc.relation.ispartofAtmospheric Environment
dc.relation.ispartofjcr3.708
dc.relation.ispartofsjr1,523
dc.rights.accessRightsAcesso restrito
dc.sourceWeb of Science
dc.subjectsmolderingpt
dc.subjectbiomass combustionpt
dc.subjectdeforestation firept
dc.titleLog smoldering after an Amazonian deforestation fireen
dc.typeArtigo
dcterms.licensehttp://www.elsevier.com/about/open-access/open-access-policies/article-posting-policy
dcterms.rightsHolderElsevier B.V.
dspace.entity.typePublication
unesp.campusUniversidade Estadual Paulista (UNESP), Faculdade de Engenharia, Guaratinguetápt
unesp.departmentEnergia - FEGpt

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