²⁴⁰Pu/²³⁹Pu signatures allow refining the chronology of radionuclide fallout in South America

dc.contributor.authorChaboche, Pierre-Alexis
dc.contributor.authorPointurier, Fabien
dc.contributor.authorSabatier, Pierre
dc.contributor.authorFoucher, Anthony
dc.contributor.authorTiecher, Tales
dc.contributor.authorMinella, Jean P.G.
dc.contributor.authorTassano, Marcos
dc.contributor.authorHubert, Amélie
dc.contributor.authorMorera Julca, Sergio Byron
dc.contributor.authorGuédron, Stéphane
dc.contributor.authorArdois, Christophe
dc.contributor.authorBoulet, Béatrice
dc.contributor.authorCossonnet, Catherine
dc.contributor.authorCabral, Pablo
dc.contributor.authorCabrera, Mirel
dc.contributor.authorChalar, Guillermo
dc.contributor.authorEvrard, Olivier
dc.coverage.spatialSouth America
dc.date.accessioned2023-04-03T16:37:51Z
dc.date.available2023-04-03T16:37:51Z
dc.date.issued2022-10-15
dc.description.abstractAtmospheric nuclear tests (1945–1980) have led to radioactive fallout across the globe. French tests in Polynesia (1966–1974) may influence the signature of fallout in South America in addition to those conducted by USA and former USSR until 1963 in the Northern hemisphere. Here, we compiled the ²⁴⁰Pu/²³⁹Pu atom ratios reported for soils of South America and conducted additional measurements to examine their latitudinal distributions across this continent. Significantly lower ratio values were found in the 20–45° latitudinal band (0.04 to 0.13) compared to the rest of the continent (up to 0.20) and attributed to the contribution of the French atmospheric tests to the ultra-trace plutonium levels found in these soils. Based on sediment cores collected in lakes of Chile and Uruguay, we show the added value of measuring ²⁴⁰Pu/²³⁹Pu atom ratios to refine the age models of environmental archives in this region of the world.es_ES
dc.description.peer-reviewPor pareses_ES
dc.formatapplication/pdfes_ES
dc.identifier.citationChaboche, P-A., Pointurier, F., Sabatier, P., Foucher, A., Tiecher, T., Minella, J. P., ... & Evrard, O. (2022). ²⁴⁰Pu/²³⁹Pu signatures allow refining the chronology of radionuclide fallout in South America.==$Science of the Total Environment, 843,$==156943. https://doi.org/10.1016/j.scitotenv.2022.156943
dc.identifier.doihttps://doi.org/10.1016/j.scitotenv.2022.156943es_ES
dc.identifier.govdocindex-oti2018
dc.identifier.journalScience of The Total Environmentes_ES
dc.identifier.urihttp://hdl.handle.net/20.500.12816/5370
dc.language.isoenges_ES
dc.publisherElsevieres_ES
dc.relation.ispartofurn:issn:1879-1026
dc.rightsinfo:eu-repo/semantics/closedAccesses_ES
dc.subjectPlutonium isotopeses_ES
dc.subjectNuclear weapon testses_ES
dc.subjectGeochronologyes_ES
dc.subjectSoil erosiones_ES
dc.subject.ocdehttps://purl.org/pe-repo/ocde/ford#1.05.09es_ES
dc.subject.ocdehttps://purl.org/pe-repo/ocde/ford#1.05.08es_ES
dc.title²⁴⁰Pu/²³⁹Pu signatures allow refining the chronology of radionuclide fallout in South Americaes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES

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