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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorANSCHUTZ, Pierre
ORCID: 0000-0001-5331-7974
IDREF: 076300331
dc.contributor.authorBENONY, Florian
dc.contributor.authorCHARBONNIER, Céline
dc.date.accessioned2025-04-24T08:00:33Z
dc.date.available2025-04-24T08:00:33Z
dc.date.issued2024-09
dc.identifier.issn0009-2541en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/206385
dc.description.abstractEnExcessive inputs of phosphorus (P) to aquatic environments can lead to eutrophication. Adsorption of phosphate on Fe oxides is one of the main process that can limit P availability. Oxidized forms of Mn have also been suggested to play a role in P trapping. However, although a considerable number of studies have shown the relationships between the geochemistry of Fe and that of phosphates, few studies have attempted to show the direct links between Mn and P. In the present study, we studied the adsorption of phosphate on synthetized Mn(III) and Mn(IV) oxides placed under natural conditions. The aim was to compare the role of Fe and Mn oxides in phosphate adsorption. Two muddy sediments were collected in a river bed at the edge of a large agricultural area. A sandy sediment was collected downstream. A muddy and a sandy sample were taken in a coastal environment. The experiments on phosphate adsorption by sediment and Mn oxides were carried out in slurries containing in situ waters spiked with 10 μM phosphate. Control experiments without Mn-oxide addition showed that the natural sediments tested still had the capacity to adsorb phosphate, in particular due to the presence of reactive Fe(III) oxides, extractable by an ascorbate solution. The addition of Mn(III) and Mn(IV) oxides in much larger quantities than the initial quantity of Fe oxides had little impact on the rate of phosphate adsorption. For both Mn(III) and Mn(IV) oxides, the Mn/P ratio between added particulate Mn and adsorbed P was very high, with values between 260 and 1000. The Fe/P ratio of the iron oxides contained in the slurries was between 6 and 20. On average, the P adsorption capacity of the Fe oxides was 50 times greater than that of the Mn oxides. Manganese oxides are generally less abundant than iron oxides in natural environments. Mn oxides therefore play a minor role in P sequestration compared with Fe oxides. Even if there are environments where Mn oxides can concentrate, the reduction of Mn oxides and subsequent liberation of adsorbed P does not represent a major risk for eutrophication of aquatic ecosystems.
dc.language.isoENen_US
dc.subject.enEutrophication
dc.subject.enPhosphorus
dc.subject.enWatershed
dc.subject.enRiver
dc.subject.enCoastal zone
dc.subject.eniron oxides
dc.subject.enManganese oxides
dc.title.enRole of manganese oxides and oxyhydroxides in phosphate sequestration in natural aquatic environments
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.chemgeo.2024.122231en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalChemical Geologyen_US
bordeaux.page122231en_US
bordeaux.volume662en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamECOBIOCen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcecrossref
hal.identifierhal-05045039
hal.version1
hal.date.transferred2025-04-24T08:00:36Z
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exporttrue
workflow.import.sourcecrossref
dc.rights.ccCC BYen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Chemical%20Geology&rft.date=2024-09&rft.volume=662&rft.spage=122231&rft.epage=122231&rft.eissn=0009-2541&rft.issn=0009-2541&rft.au=ANSCHUTZ,%20Pierre&BENONY,%20Florian&CHARBONNIER,%20C%C3%A9line&rft.genre=article


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