N 2 O emissions and NO 3 − leaching from two contrasting regions in Austria and influence of soil, crops and climate: a modelling approach

dc.bibliographicCitation.firstPage95eng
dc.bibliographicCitation.issue1eng
dc.bibliographicCitation.journalTitleNutrient Cycling in Agroecosystemseng
dc.bibliographicCitation.lastPage111eng
dc.bibliographicCitation.volume113eng
dc.contributor.authorKasper, M.
dc.contributor.authorFoldal, C.
dc.contributor.authorKitzler, B.
dc.contributor.authorHaas, E.
dc.contributor.authorStrauss, P.
dc.contributor.authorEder, A.
dc.contributor.authorZechmeister-Boltenstern, S.
dc.contributor.authorAmon, B.
dc.date.accessioned2021-07-26T10:59:16Z
dc.date.available2021-07-26T10:59:16Z
dc.date.issued2019
dc.description.abstractNational emission inventories for UN FCCC reporting estimate regional soil nitrous oxide (N 2 O) fluxes by considering the amount of N input as the only influencing factor for N 2 O emissions. Our aim was to deepen the understanding of N 2 O fluxes from agricultural soils, including region specific soil and climate properties into the estimation of emission to find targeted mitigation measures for the reduction of nitrogen losses and GHG emissions. Within this project, N 2 O emissions and nitrate (NO 3 − ) leaching were modelled under spatially distinct environmental conditions in two agricultural regions in Austria taking into account region specific soil and climatic properties, management practices and crop rotations. The LandscapeDNDC ecosystem model was used to calculate N 2 O emissions and NO 3 − leaching reflecting different types of vegetation, management operations and crop rotations. In addition, N input and N fluxes were assessed and N 2 O emissions were calculated. This approach allowed identifying hot spots of N 2 O emissions. Results show that certain combinations of soil type, weather conditions, crop and management can lead to high emissions. Mean values ranged from 0.15 to 1.29 kg N 2 O–N ha −1  year −1 (Marchfeld) and 0.26 to 0.52 kg N 2 O–N ha −1  year −1 (Grieskirchen). Nitrate leaching, which strongly dominated N-losses, often reacted opposite to N 2 O emissions. Larger quantities of NO 3 − were lost during years of higher precipitation, especially if winter barley was cultivated on sandy soils. Taking into account the detected hot spots of N 2 O emissions and NO 3 − leaching most efficient measures can be addressed to mitigate environmental impacts while maximising crop production. © 2018, The Author(s).eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/6362
dc.identifier.urihttps://doi.org/10.34657/5409
dc.language.isoengeng
dc.publisherDordrecht [u.a.] : Springer Science + Business Media B.Veng
dc.relation.doihttps://doi.org/10.1007/s10705-018-9965-z
dc.relation.essn1573-0867
dc.relation.issn0167-1731
dc.relation.issn1385-1314
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subject.ddc570eng
dc.subject.otherAgricultureeng
dc.subject.otherCrop rotationeng
dc.subject.otherCultivationeng
dc.subject.otherN 2 O emissionseng
dc.subject.otherNO 3 − leachingeng
dc.titleN 2 O emissions and NO 3 − leaching from two contrasting regions in Austria and influence of soil, crops and climate: a modelling approacheng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccesseng
wgl.contributorATBeng
wgl.subjectBiowissensschaften/Biologieeng
wgl.typeZeitschriftenartikeleng
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