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Spatial and temporal variability of surface water and groundwater before and after the remediation of a Portuguese uranium mine area

dc.contributor.authorNeiva, A.M.R.
dc.contributor.authorCarvalho, Paula
dc.contributor.authorAntunes, I.M.H.R.
dc.contributor.authorSantos, A.C.T.
dc.contributor.authorPinto, M.M.S.C.
dc.date.accessioned2015-11-25T13:34:10Z
dc.date.available2015-11-25T13:34:10Z
dc.date.issued2015
dc.description.abstractThe old Senhora das Fontes uranium mine, in central Portugal, consists of quartz veins which penetrated along fracture shear zones at the contact between graphite schist and orthogneiss. The mine was exploited underground until a depth of 90 m and was closed down in 1971. The ores from this mine and two others were treated in the mine area by the heap-leach process which ended in 1982. Seven dumps containing a total of about 33,800 m3 of material and partially covered by natural vegetation were left in the mine area. A remediation process took place from May 2010 to January 2011. The material deposited in dumps was relocated and covered with erosion resisting covers. Surface water and groundwater were collected in the wet season just before the remediation, in the following season at the beginning of the remediation and also after the remediation in the following dry season. Before, at the beginning and after the remediation, surface water and groundwater have an acid-to-alkaline pH, which decreased with the remediation, whereas Eh increased. In general, before the remediation, uranium concentration was up to 83 μg/L in surface water and up to 116 μg/L in groundwater, whereas at the beginning of the remediation it increases up to 183 μg/L and 272 μg/L in the former and the latter, respectively, due to the remobilization of mine dumps and pyrite and chalcopyrite exposures, responsible for the pH decrease. In general, after the remediation, the U concentration decreased significantly in surface water and groundwater at the north part of the mine area, but increased in both, particularly in the latter up to 774 μg/L in the south and southwest parts of this area, attributed to the remobilization of sulphides that caused mobilization of metals and arsenic which migrated to the groundwater flow. Uranium is adsorbed in clay minerals, but also in goethite as indicated by the geochemical modelling. After the remediation, the saturation indices of oxyhydroxides decrease as pH decreases. The remediation also caused decrease in Cd, Co, Cr, Ni, Pb, Zn, Cu, As, Sr and Mn concentrations of surface water and groundwater, particularly in the north part of the mine area, which is supported by the speciation modelling that shows the decrease of most dissolved bivalent species. However, in general, after the remediation, Th, Cd, Al, Li, Pb, Sr and As concentrations increased in groundwater and surface water at south and southwest of the mine area. Before and after the remediation, surface water and groundwater are contaminated in U, Cd, Cr, Al, Mn, Ni, Pb, Cu and As. Remediation caused only some improvement at north of the mine area, because at south and southwest part, after the remediation, the groundwater is more contaminated than before the remediation.pt_PT
dc.identifier.citationNEIVA, A.M.R. [et al.] (2015) - Spatial and temporal variability of surface water and groundwater before and after the remediation of a Portuguese uranium mine area. Chemie der Erde. ISSN 0009-2819. 75, p. 345-356.pt_PT
dc.identifier.doi10.1016/j.chemer.2015.06.001pt_PT
dc.identifier.issn0009-2819
dc.identifier.urihttp://hdl.handle.net/10400.11/3108
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherElsevierpt_PT
dc.relation.publisherversionhttp://www.sciencedirect.com/science/article/pii/S0009281915000434pt_PT
dc.subjectUraniumpt_PT
dc.subjectMine areapt_PT
dc.subjectSurface waterpt_PT
dc.subjectGroundwaterpt_PT
dc.subjectSpatial distribution;pt_PT
dc.subjectBefore remediationpt_PT
dc.subjectAfter remediationpt_PT
dc.subjectGeochemical modellingpt_PT
dc.subjectContaminationpt_PT
dc.subjectCentral Portugalpt_PT
dc.titleSpatial and temporal variability of surface water and groundwater before and after the remediation of a Portuguese uranium mine areapt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.endPage356pt_PT
oaire.citation.startPage345pt_PT
oaire.citation.titleChemir der Erdept_PT
oaire.citation.volume75pt_PT
person.familyNameCarvalho
person.familyNameantunes
person.givenNamePaula
person.givenNameIsabel Margarida
person.identifier.ciencia-idCB1E-FAD2-37D6
person.identifier.orcid0000-0002-3767-5410
person.identifier.orcid0000-0003-3456-5926
person.identifier.ridM-1043-2013
person.identifier.scopus-author-id6701817085
rcaap.rightsrestrictedAccesspt_PT
rcaap.typearticlept_PT
relation.isAuthorOfPublicationf3f92fb6-6841-483f-b6bc-68dcb84b64f8
relation.isAuthorOfPublication1db83c95-f80c-41bb-b5c6-437ab32d9683
relation.isAuthorOfPublication.latestForDiscoveryf3f92fb6-6841-483f-b6bc-68dcb84b64f8

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