Rodyti trumpą aprašą

dc.contributor.authorda Silva Pereira, Paulo Alexandre
dc.contributor.authorÚbeda, Xavier
dc.contributor.authorMartin, Deborah
dc.date.accessioned2023-09-18T18:45:37Z
dc.date.available2023-09-18T18:45:37Z
dc.date.issued2011
dc.identifier.issn2029-7106
dc.identifier.other(BIS)VGT02-000023172
dc.identifier.urihttps://etalpykla.vilniustech.lt/handle/123456789/131578
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.eng
dc.format.extentp. 255-262
dc.format.mediumtekstas / txt
dc.language.isoeng
dc.relation.isreferencedbyConference Proceedings Citation Index - Science (Web of Science)
dc.titleSpatial variation of ash total carbon and total nitrogen after a wildfire
dc.typeStraipsnis konferencijos darbų leidinyje Web of Science DB / Paper in conference publication in Web of Science DB
dcterms.references39
dc.type.pubtypeP1a - Straipsnis konferencijos darbų leidinyje Web of Science DB / Article in conference proceedings Web of Science DB
dc.contributor.institutionVilniaus Gedimino technikos universitetas
dc.contributor.institutionUniversity of Barcelona
dc.contributor.institutionU.S. Geological Survey, Boulder
dc.contributor.facultyAplinkos inžinerijos fakultetas / Faculty of Environmental Engineering
dc.subject.researchfieldN 012 - Ekologija ir aplinkotyra / Ecology and environmental studies
dc.subject.researchfieldT 004 - Aplinkos inžinerija / Environmental engineering
dc.subject.enTotal carbon
dc.subject.enTotal nitrogen
dc.subject.enWildfire
dc.subject.enFire severity
dc.subject.enInterpolation methods
dc.subject.enSpatial distribution
dcterms.sourcetitle8th International Conference "Environmental Engineering", May 19-20, 2011, Vilnius, Lithuania : selected papers. Vol. 1. Environmental protection
dc.publisher.nameTechnika
dc.publisher.cityVilnius
dc.identifier.doiMRU02-000010874
dc.identifier.doi000307743800045
dc.identifier.elaba3952612


Šio įrašo failai

FailaiDydisFormatasPeržiūra

Su šiuo įrašu susijusių failų nėra.

Šis įrašas yra šioje (-se) kolekcijoje (-ose)

Rodyti trumpą aprašą