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dc.contributor.authorMarcos Porras, Elena María
dc.contributor.authorFernández García, Víctor
dc.contributor.authorFernández Manso, Alfonso
dc.contributor.authorQuintano Pastor, María del Carmen 
dc.contributor.authorValbuena, Luz
dc.contributor.authorTárrega, Reyes
dc.contributor.authorEstanislao, Luis Calabuig
dc.contributor.authorCalvo, Leonor
dc.date.accessioned2022-10-27T12:39:08Z
dc.date.available2022-10-27T12:39:08Z
dc.date.issued2018
dc.identifier.citationForests, 2018, vol.9, n. 8, p. 494es
dc.identifier.urihttps://uvadoc.uva.es/handle/10324/56585
dc.descriptionProducción Científicaes
dc.description.abstractWe analysed the relationship between burn severity indicators, from remote sensing and field observations, and soil properties after a wildfire in a fire-prone Mediterranean ecosystem. Our study area was a large wildfire in a Pinus pinaster forest. Burn severity from remote sensing was identified by studying immediate post-fire Land Surface Temperature (LST). We also evaluated burn severity in the field applying the Composite Burn Index (CBI) in a total of 84 plots (30 m diameter). In each plot we evaluated litter consumption, ash colour and char depth as visual indicators. We collected soil samples and pH, soil organic carbon, dry aggregate size distribution (MWD), aggregate stability and water repellency were analysed. A controlled heating of soil was also carried out in the laboratory, with soil from the control plots, to compare with the changes produced in soils affected by different severity levels in the field. Our results shown that changes in soil properties affected by wildfire were only observed in soil aggregation in the high severity situation. The laboratory-controlled heating showed that temperatures of about 300 ◦C result in a significant reduction in soil organic carbon and MWD. Furthermore, soil organic carbon showed a significant decrease when LST values increased. Char depth was the best visual indicator to show changes in soil properties (mainly physical properties) in large fires that occur in Mediterranean pine forests. We conclude that CBI and post-fire LST can be considered good indicators of soil burn severity since both indicate the impact of fire on soil properties.es
dc.format.mimetypeapplication/pdfes
dc.language.isoenges
dc.publisherMDPIes
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/*
dc.subject.classificationPine forestes
dc.subject.classificationWildfirees
dc.subject.classificationSoil burn severityes
dc.subject.classificationControlled heatinges
dc.titleEvaluation of composite burn index and land surface temperature for assessing soil burn severity in mediterranean fire-prone pine ecosystemses
dc.typeinfo:eu-repo/semantics/articlees
dc.rights.holder© 2018 The Author(s)es
dc.identifier.doi10.3390/f9080494es
dc.relation.publisherversionhttps://www.mdpi.com/1999-4907/9/8/494es
dc.identifier.publicationfirstpage494es
dc.identifier.publicationissue8es
dc.identifier.publicationtitleForestses
dc.identifier.publicationvolume9es
dc.peerreviewedSIes
dc.description.projectMinisterio de Economía y Competitividad y el Fondo Europeo de Desarrollo Regional (FEDER), en el marco del proyecto GESFIRE (AGL2013-48189-C2-1-R)es
dc.description.projectJunta de Castilla y León en el marco del proyecto SEFIRECYL (LE001P17)es
dc.identifier.essn1999-4907es
dc.rightsAtribución 4.0 Internacional*
dc.type.hasVersioninfo:eu-repo/semantics/publishedVersiones
dc.subject.unesco31 Ciencias Agrariases
dc.subject.unesco3106 Ciencia Forestales


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