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hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorCORNU, Jean-Yves
hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorDENAIX, Laurence
hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorLACOSTE, Julien
hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorSAPPIN-DIDIER, Valérie
hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorNGUYEN, Christophe
hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorSCHNEIDER, André
dc.date.accessioned2024-04-08T12:11:30Z
dc.date.available2024-04-08T12:11:30Z
dc.date.issued2016
dc.identifier.issn0944-1344
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/196692
dc.description.abstractEnPredicting the soil-to-plant transfer of metals in the context of global warming has become a major issue for food safety. It requires a better understanding of how the temperature alters the bioavailability of metals in cultivated soils. This study focuses on one agricultural soil contaminated by Cd, Zn and Pb. DGT measurements were performed at 10, 20 and 30°C to assess how the bioavailability of metals was affected by a rise in soil temperature. A lettuce crop was cultivated in the same conditions to determine if the soil-to-plant transfer of metals increased with a rise in soil temperature. A gradual decline in Cd and Zn bioavailability was observed from 10 to 30°C, which was attributed to more intense complexation of metals in the pore water at higher temperatures. Together with its aromaticity, the affinity of dissolved organic matter (DOM) for metals was indeed suspected to increase with soil temperature. One main output of the present work is a model which satisfactorily explains the thermal-induced changes in the characteristics of DOM reported in Cornu et al. (Geoderma 162:65-70, 2011) by assuming that the mineralization of initial aliphatic compounds followed a first-order reaction, increased with soil temperature according to the Arrhenius law, and due to a priming effect, led to the appearance of aromatic molecules. The soil-to-plant transfer of Cd and Zn was promoted at higher soil temperatures despite a parallel decrease in Cd and Zn bioavailability. This suggests that plant processes affect the soil-to-plant transfer of Cd and Zn the most when the soil temperature rises.
dc.language.isoen
dc.publisherSpringer Verlag
dc.subjectsécurité alimentaire
dc.subjectaccumulation du cadmium
dc.subjectbioaccumulation
dc.subjectcontamination
dc.subjectzinc
dc.subjectplomb
dc.subjectsol agricole
dc.subject.enaromatic ligand
dc.subject.enbioavailability
dc.subject.enfood safety
dc.subject.englobal warwing
dc.subject.enmetal
dc.subject.enmodelling
dc.subject.enbiomagnification
dc.subject.enlead
dc.subject.enagricultural soil
dc.title.enImpact of temperature on the dynamics of organic matter and on the soil-to-plant transfer of Cd, Zn and Pb in a contaminated agricultural soil
dc.typeArticle de revue
dc.identifier.doi10.1007/s11356-015-5432-4
dc.subject.halSciences du Vivant [q-bio]/Toxicologie/Ecotoxicologie
dc.subject.halSciences du Vivant [q-bio]/Sciences agricoles
bordeaux.journalEnvironmental Science and Pollution Research
bordeaux.page2997-3007
bordeaux.volume23
bordeaux.hal.laboratoriesInteractions Soil Plant Atmosphere (ISPA) - UMR 1391*
bordeaux.issue4
bordeaux.institutionBordeaux Sciences Agro
bordeaux.institutionINRAE
bordeaux.peerReviewedoui
hal.identifierhal-01512161
hal.version1
hal.popularnon
hal.audienceNon spécifiée
hal.origin.linkhttps://hal.archives-ouvertes.fr//hal-01512161v1
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