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Soil ozone deposition: Dependence of soil resistance to soil texture

hal.structure.identifierSciences pour l'Action et le Développement : Activités, Produits, Territoires [SADAPT]
dc.contributor.authorSTELLA, Patrick
hal.structure.identifierEcologie fonctionnelle et écotoxicologie des agroécosystèmes [ECOSYS]
dc.contributor.authorLOUBET, Benjamin
hal.structure.identifierUnité Expérimentale Fourrages et Environnement de Lusignan [UEFE]
dc.contributor.authorDE BERRANGER, Christophe
hal.structure.identifierUnité Expérimentale Fourrages et Environnement de Lusignan [UEFE]
dc.contributor.authorCHARRIER, Xavier
hal.structure.identifierCentre d'études spatiales de la biosphère [CESBIO]
dc.contributor.authorCESCHIA, Eric
hal.structure.identifierUniversità cattolica del Sacro Cuore [Brescia] [Unicatt]
dc.contributor.authorGEROSA, Giacomo
hal.structure.identifierUniversità cattolica del Sacro Cuore [Brescia] [Unicatt]
dc.contributor.authorFINCO, Angelo
hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorLAMAUD, Eric
hal.structure.identifierLaboratoire d'aérologie [LAERO]
dc.contributor.authorSERÇA, Dominique
hal.structure.identifierInstitut de recherches sur la catalyse et l'environnement de Lyon [IRCELYON]
dc.contributor.authorGEORGE, Christian
hal.structure.identifierEcologie fonctionnelle et écotoxicologie des agroécosystèmes [ECOSYS]
dc.contributor.authorCIURARU, Raluca
dc.date.accessioned2024-04-08T11:50:42Z
dc.date.available2024-04-08T11:50:42Z
dc.date.issued2019
dc.identifier.issn1352-2310
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/195398
dc.description.abstractEnSoil deposition is an essential pathway for tropospheric ozone (O3) removal, but its controlling factors remain unclear. Here, we explored the variability of soil O3 resistance in response to soil texture. To this aim, data of O3 deposition over bare soil obtained from micrometeorological measurements under contrasted meteorological conditions for five sites were used. The results obtained are twofold: (i) soil resistance (Rsoil) increased with soil surface relative humidity (RHsurf), but (ii) this relationship exhibited large site-by-site variability. Further analysis showed that the minimum soil resistance (corresponding to completely dry soil surface or RHsurf = 0%) and the increase of Rsoil with RHsurf are both linked to soil clay content. These results can be explained by (i) the soil surface available for O3 deposition at a microscopic scale which is a function of the soil specific surface area, and (ii) the capacity of a soil to adsorb water according to its clay content and therefore to reduce the surface active for O3 deposition. From these results, a new parameterization has been established to estimate Rsoil as a function of RHsurf and soil clay fraction.
dc.language.isoen
dc.publisherElsevier
dc.rights.urihttp://creativecommons.org/licenses/by/
dc.subject.enRelative humidity
dc.subject.enClay content
dc.subject.enOzone
dc.subject.enSoil resistance
dc.title.enSoil ozone deposition: Dependence of soil resistance to soil texture
dc.typeArticle de revue
dc.identifier.doi10.1016/j.atmosenv.2018.11.036
dc.subject.halSciences du Vivant [q-bio]
bordeaux.journalAtmospheric Environment
bordeaux.page202-209
bordeaux.volume199
bordeaux.hal.laboratoriesInteractions Soil Plant Atmosphere (ISPA) - UMR 1391*
bordeaux.institutionBordeaux Sciences Agro
bordeaux.institutionINRAE
bordeaux.peerReviewedoui
hal.identifierhal-01933639
hal.version1
hal.popularnon
hal.audienceNon spécifiée
hal.origin.linkhttps://hal.archives-ouvertes.fr//hal-01933639v1
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Atmospheric%20Environment&rft.date=2019&rft.volume=199&rft.spage=202-209&rft.epage=202-209&rft.eissn=1352-2310&rft.issn=1352-2310&rft.au=STELLA,%20Patrick&LOUBET,%20Benjamin&DE%20BERRANGER,%20Christophe&CHARRIER,%20Xavier&CESCHIA,%20Eric&rft.genre=article


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