Rodyti trumpą aprašą

dc.contributor.authorPereira, Paulo
dc.contributor.authorUbeda, Xavier
dc.contributor.authorMartin, Deborah
dc.date.accessioned2026-04-15T13:17:13Z
dc.date.available2026-04-15T13:17:13Z
dc.date.issued2011
dc.identifier.isbn9789955288268en_US
dc.identifier.issn2029-7106en_US
dc.identifier.urihttps://etalpykla.vilniustech.lt/handle/123456789/160259
dc.description.abstractThe present work aims to study the spatial variability of ash Total Carbon (TC%) and Total Nitrogen (TN%) after a wildfire occurred in Portugal. Ash TC% a mean of 26.72 % (±8.76 %) and ash TN% of 1.20 % (±0.32 %). We observed that the area recover very fast to wildfire and two years the great part of soil was cover by vegetation. The fire severity (assessed with ash color and CaCO3 content) was more related with ash TC%, than ash TN% due the different vulnerability and response of these two elements to fire temperature and as consequence severity. Previous to model data we tested their normality that only was achieved in the case of TC% after a neperian logarithmic transformation (ln). TN% respected gaussian distribution, however showed a high skewness, thus this variable was also ln transformed. Ash TC%(ln) presented an excellent spatial structure and the experimental model fits better with the rational quadratic model and ash TN%(ln) with the lineal model. Among all interpolation methods tested, the most accurate to interpolate ash TC%(ln) was IDW2 and the less suitable LP3. In relation to ash TN%(ln) the best interpolation technique was SPT and the less precise LP3. This allow us to observe differences that the spatial distribution of both variables is different, that is due the small scale variability observed in ash TC%(ln). In general the models were well performed because the residuals mean were closed to 0 and no differences between average of predicted and estimated values were identified. Ash TC%(ln) spatial distribution was in higher amounts in western, northern part and southeast and northeast corner of the plot and lower in the centre and south of the interested area and ash TN%(ln) was observed in higher amounts in the southwest and southeast part of the plot and lesser in the central part.en_US
dc.description.sponsorshipSpanish Ministry of Science and Technologyen_US
dc.description.sponsorshipEuropean Regional Development Funden_US
dc.description.sponsorshipServeis Científico-Tècnics from the University of Barcelonaen_US
dc.format.extent8 p.en_US
dc.format.mediumTekstas / Texten_US
dc.language.isoenen_US
dc.relation.urihttps://etalpykla.vilniustech.lt/handle/123456789/160185en_US
dc.source.urihttp://enviro2011.vgtu.lt/Abstracts/1/045.htmlen_US
dc.subjectTotal Carbonen_US
dc.subjectTotal Nitrogenen_US
dc.subjectWildfireen_US
dc.subjectFire Severityen_US
dc.subjectInterpolation Methodsen_US
dc.subjectSpatial Distributionen_US
dc.titleSpatial variation of ash total carbon and total nitrogen after a wildfireen_US
dc.typeKonferencijos publikacija / Conference paperen_US
dcterms.accessRightsLaisvai prieinamas / Openly availableen_US
dcterms.accrualMethodRankinis pateikimas / Manual submissionen_US
dcterms.alternativeEnvironmental Protectionen_US
dcterms.issued2011-05-20
dcterms.references39en_US
dc.description.versionTaip / Yesen_US
dc.contributor.institutionVilniaus Gedimino technikos universitetasen_US
dc.contributor.institutionVilnius Gediminas Technical Universityen_US
dc.contributor.institutionUniversity of Barcelonaen_US
dc.contributor.institutionU.S. Geological Surveyen_US
dcterms.sourcetitle8th International Conference “Environmental Engineering” (ICEE-2011)en_US
dc.identifier.eisbn9789955288275en_US
dc.identifier.eissn2029-7092en_US
dc.publisher.nameVilnius Gediminas Technical Universityen_US
dc.publisher.nameVilniaus Gedimino technikos universitetasen_US
dc.publisher.countryLithuaniaen_US
dc.publisher.countryLietuvaen_US
dc.publisher.cityVilniusen_US
dc.description.grantnameEvaluation of the quality of Mediterranean soils affected by fire in a middle and large termen_US
dc.description.grantnumberCGL2006-11107-C0202/BOSen_US


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