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dc.contributor.editorDing, Shiminges
dc.creatorPeñuela Fernández, Andréses
dc.creatorHurtado Bermúdez, Santiago Josées
dc.creatorGarcía Gamero, Vanesaes
dc.creatorMás Balbuena, José Luises
dc.creatorKetterer, M. E.es
dc.creatorVanwalleghem, Tomes
dc.creatorGómez Calero, José Alfonsoes
dc.date.accessioned2023-07-21T10:32:55Z
dc.date.available2023-07-21T10:32:55Z
dc.date.issued2023-06-01
dc.identifier.citationPeñuela Fernández, A., Hurtado Bermúdez, S.J., García Gamero, V., Más Balbuena, J.L., Ketterer, M.E., Vanwalleghem, T. y Gómez Calero, J.A. (2023). A comparison of 210Pbxs, 137Cs, and Pu isotopes as proxies of soil redistribution in South Spain under severe erosion conditions. Journal of Soils and Sediments, 2023. https://doi.org/10.1007/s11368-023-03560-5.
dc.identifier.issn1439-0108es
dc.identifier.issn1614-7480es
dc.identifier.urihttps://hdl.handle.net/11441/148153
dc.descriptionLicencia CC BY 4.0es
dc.description.abstractPurpose The use of fallout radionuclides as proxies for the study of soil redistribution processes in semiarid environments of Southern Spain has been restricted to 137Cs. The potential and limitations of alternative proxies such as 239+240Pu and 210Pbxs should be explored given the expected constrains imposed by the features of the study area. Materials and methods Four soil and one sediment cores were collected in a highly eroded area to test the feasibility of these proxies under demanding conditions. The use of gamma spectrometry and ICP-MS did allow exploring the potential of 210Pbxs and Pu isotopes against the well-established tracer, 137Cs. The activity ratios 239+240Pu/137Cs were explored to evaluate the previous evolution of the sampling sites. Soil redistribution rates were estimated using the model MODERN. Results and discussion Despite all the profles showed intense perturbation, Pu isotopes showed the highest potential thanks to higher sensitivity and sample throughput. The deviations of 239+240Pu/137Cs inventory ratios (0.012–0.158) from the global fallout average (0.026±0.003) suggest that the sediment core was a deposition site involving alternate episodes of topsoil removal and incorporation from diferent sources. The calculated erosion rates ranged 34–43 t ha−1 year−1, being in good agreement for 137Cs and 239+240Pu. 210Pbxs was not used due to low-quality data. Conclusions The use of Pu as a tracer of soil redistribution processes in semiarid areas seems to be promising even under severe erosion conditions. The use of 210Pbxs is not recommended in this area due to its low concentration.es
dc.formatapplication/pdfes
dc.format.extent19 p.es
dc.language.isoenges
dc.publisherSpringeres
dc.relation.ispartofJournal of Soils and Sediments, 2023.
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectIsotopeses
dc.subjectSoil redistributiones
dc.subjectSevere erosion conditionses
dc.titleA comparison of 210Pbxs, 137Cs, and Pu isotopes as proxies of soil redistribution in South Spain under severe erosion conditionses
dc.typeinfo:eu-repo/semantics/articlees
dcterms.identifierhttps://ror.org/03yxnpp24
dc.type.versioninfo:eu-repo/semantics/publishedVersiones
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses
dc.contributor.affiliationUniversidad de Sevilla. Departamento de Física Aplicada IIes
dc.contributor.affiliationUniversidad de Sevilla. Departamento de Física Aplicada I
dc.relation.projectIDFIS2015-69673-Pes
dc.relation.projectIDPID2019-109924RB-I00es
dc.relation.projectIDVI PPI-ID SOL2017-9049es
dc.relation.publisherversionhttps://link.springer.com/article/10.1007/s11368-023-03560-5es
dc.identifier.doi10.1007/s11368-023-03560-5es
dc.contributor.groupUniversidad de Sevilla. RNM138: Física Nuclear Aplicadaes
dc.journaltitleJournal of Soils and Sedimentses
dc.publication.volumen2023es
dc.contributor.funderMinisterio de Ciencia, Innovación y Universidades (MICINN). Españaes
dc.contributor.funderUniversidad de Sevillaes

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