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Stream sediments as a repository of U, Th and As around abandoned uranium mines in central Portugal: implications for water quality management

dc.contributor.authorCarvalho, Paula
dc.contributor.authorAntunes, I.M.H.R.
dc.contributor.authorAlbuquerque, M.T.D.
dc.contributor.authorSantos, António
dc.contributor.authorCunha, Pedro Proença
dc.date.accessioned2022-03-23T10:46:05Z
dc.date.available2024-01-01T01:31:03Z
dc.date.issued2022
dc.description.abstractThis work focuses on the study of water–sediment interaction around abandoned uranium mines with open-pit lakes and mine dumps. Nineteen water and eleven stream sediment samples were collected in the abandoned Barrôco D. Frango mine, central Portugal. The trace element distribution was compared with other abandoned uranium mines in Portugal and worldwide. Generally, U, Th, and As contents in the open-pit water are high and similar to those of downstream water, suggesting its influence on aquatic systems. In abandoned mines with small to medium U exploitation, the stream sediments are moderately to heavily contaminated with U, Th and As, being U and As the most important contaminants, confirmed by their partition coefficients. A moderate to considerable potential ecological risk (34–79) was found around the abandoned Barrôco D. Frango mine area, mainly due to As contents in stream sediments. Water and stream sediments from abandoned U mines worldwide have U levels of up to 436 μg/L and 5024 mg/kg, respectively, while those from Barrôco D. Frango have 37.3 μg/L and 189 mg/kg, respectively. However, the longer the distance from the Barrôco D. Frango open-pit lake and mine dump, the higher U, Th and As contents in stream sediments, which is a warning indicator. Cluster heat maps of the water composition from four abandoned uranium mine areas show that Mondego Sul and Barrôco D. Frango mines are the most geochemically similar. Results show that stream sediments should be included in water quality management and future remediation plans of abandoned uranium mines.pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.citationCARVALHO, Paula [et al.] (2022) - Stream sediments as a repository of U, Th and As around abandoned uranium mines in central Portugal: implications for water quality management. Environmental Earth Sciences. 81. DOI: 10.1007/s12665-022-10275-2
dc.identifier.doi10.1007/s12665-022-10275-2pt_PT
dc.identifier.urihttp://hdl.handle.net/10400.11/7927
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherSpringerpt_PT
dc.relationUID/GEO/04035/2016 - GeoBioTec- GeoBioSciences, GeoTechnologies and GeoEngineeringpt_PT
dc.relationUIDB/04683/2020 - ICTpt_PT
dc.relationUIDP/04683/2020 - ICTpt_PT
dc.relationUIDB/MAR/04292/2020 - MARE (Marine and Environmental Sciences Centre)pt_PT
dc.subjectWater–sediment interactionpt_PT
dc.subjectQuality indicatorspt_PT
dc.subjectEcological riskpt_PT
dc.subjectArsenicpt_PT
dc.subjectUranium minespt_PT
dc.titleStream sediments as a repository of U, Th and As around abandoned uranium mines in central Portugal: implications for water quality managementpt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.issue6pt_PT
oaire.citation.titleEnvironmental Earth Sciencespt_PT
oaire.citation.volume81pt_PT
person.familyNameCarvalho
person.familyNameantunes
person.familyNameAlbuquerque
person.givenNamePaula
person.givenNameIsabel Margarida
person.givenNameMaria Teresa
person.identifier.ciencia-idCB1E-FAD2-37D6
person.identifier.ciencia-id5A1C-8956-4C0A
person.identifier.orcid0000-0002-3767-5410
person.identifier.orcid0000-0003-3456-5926
person.identifier.orcid0000-0002-8782-6133
person.identifier.ridM-1043-2013
person.identifier.ridB-1536-2013
person.identifier.scopus-author-id6701817085
person.identifier.scopus-author-id55507421600
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT
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relation.isAuthorOfPublication1db83c95-f80c-41bb-b5c6-437ab32d9683
relation.isAuthorOfPublicatione2c2d171-e148-4c23-9cf8-0eb6d810c15e
relation.isAuthorOfPublication.latestForDiscoverye2c2d171-e148-4c23-9cf8-0eb6d810c15e

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