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hal.structure.identifierEcologie fonctionnelle et écotoxicologie des agroécosystèmes [ECOSYS]
dc.contributor.authorPOTIER, Elise
hal.structure.identifierEcologie fonctionnelle et écotoxicologie des agroécosystèmes [ECOSYS]
dc.contributor.authorLOUBET, Benjamin
hal.structure.identifierEcologie fonctionnelle et écotoxicologie des agroécosystèmes [ECOSYS]
dc.contributor.authorDURAND, Brigitte
hal.structure.identifierEcologie fonctionnelle et écotoxicologie des agroécosystèmes [ECOSYS]
dc.contributor.authorFLURA, Dominique
hal.structure.identifierEcologie fonctionnelle et écotoxicologie des agroécosystèmes [ECOSYS]
dc.contributor.authorDESCHAMPS, Marjolaine
hal.structure.identifierEcologie fonctionnelle et écotoxicologie des agroécosystèmes [ECOSYS]
dc.contributor.authorCIURARU, Raluca
hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorOGÉE, Jérôme
dc.date.accessioned2024-04-08T12:05:30Z
dc.date.available2024-04-08T12:05:30Z
dc.date.issued2017
dc.identifier.issn1352-2310
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/196360
dc.description.abstractEnIn this study we present results from a laboratory experiment designed to evaluate the first-order chemical reaction rate (k) of ozone in water films on plant leaves occurring during dew or rain events. Ozone deposition to wet cuticles is indeed known to be a significant pathway of ozone deposition, but the underlying processes are not yet well understood. Leaf infusions obtained by infusing plant leaves with water at room temperature were introduced into a wet effluent denuder fed with a flux of ozone-rich air. Ozone, water vapour concentrations and temperature were measured in both inlet and outlet airflows in order to compute ozone reaction rates kr using an ozone reaction-diffusion model in the water film. Ascorbate solutions were used to validate the set up and led to kr = 3.6 107 M−1 s−1 consistent with the literature. Ozone reaction rates were determined for wheat, beech, oak and pine leaves infusions at several developmental stages were, as well as for rain samples. Leaf infusions reaction rates were between 240 s−1 and 3.4 105 s−1 depending on species and developmental stage, while kr for rain water range from 130 to 830 s−1. Wheat leaves solutions showed significantly (P < 0.001) higher kr (median 73800 s−1) compared to the other tree species (median 4560 s−1). Senescing or dead leaves also showed significantly (P < 0.001) larger kr (median 21100 s−1) compared to non-senescent leaves (median 3200 s−1). In wheat, kr also increased with increasing yellow leaf fraction. Our results are in the range of previously reported ozone deposition on wet leaves in field or chamber studies. Composition of leaves infusions and previous studies on throughfall and dew composition shows that reaction of ozone with inorganic compounds may only explain the smallest measured kr. The largest kr observed during senescent are most likely due to reaction with organic material. This is confirmed by our LC-MS measurements which showed detection of ascorbate and VOCs as well as the reaction products of ozone with these compounds.
dc.language.isoen
dc.publisherElsevier
dc.rights.urihttp://creativecommons.org/licenses/by/
dc.subjectozone
dc.subjectréaction chimique
dc.subjectsurface foliaire
dc.subject.enozone deposition
dc.subject.enascorbate
dc.subject.encuticle
dc.subject.enwater film
dc.subject.ensenescence
dc.subject.entropospheric ozone
dc.subject.enchemical reaction
dc.subject.enleaf area
dc.title.enChemical reaction rates of ozone in water infusions of wheat, beech, oak and pine leaves of different ages
dc.typeArticle de revue
dc.identifier.doi10.1016/j.atmosenv.2016.11.069
dc.subject.halSciences de l'environnement/Milieux et Changements globaux
bordeaux.journalAtmospheric Environment
bordeaux.page176-187
bordeaux.volume151
bordeaux.hal.laboratoriesInteractions Soil Plant Atmosphere (ISPA) - UMR 1391*
bordeaux.institutionBordeaux Sciences Agro
bordeaux.institutionINRAE
bordeaux.peerReviewedoui
hal.identifierhal-01519142
hal.version1
hal.popularnon
hal.audienceNon spécifiée
hal.origin.linkhttps://hal.archives-ouvertes.fr//hal-01519142v1
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Atmospheric%20Environment&rft.date=2017&rft.volume=151&rft.spage=176-187&rft.epage=176-187&rft.eissn=1352-2310&rft.issn=1352-2310&rft.au=POTIER,%20Elise&LOUBET,%20Benjamin&DURAND,%20Brigitte&FLURA,%20Dominique&DESCHAMPS,%20Marjolaine&rft.genre=article


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