Factores de enriquecimiento metálico en sedimentos holocenos del estuario del río Tinto (SO de España)

dc.contributor.authorLópez González, Nieves
dc.contributor.authorBorrego Flores, José
dc.contributor.authorCarro Flores, Berta
dc.contributor.authorLozano Soria, O.
dc.date.accessioned2014-10-16T09:40:44Z
dc.date.available2014-10-16T09:40:44Z
dc.date.issued2004
dc.description.abstractMetal concentration in sediments samples from two vibracores in the Tinto river estuary it has been determined. The enrichment factors (EF) of metal associated to sulphide deposits (Fe, Cu, Zn, Pb and As), in most cases, is over 2. Cu, Zn and As have much higher EF, over 10 in surficial samples. The progressive shallowness of the estuary has undergone a relative increase in acidic river water volume with respect to seawater. This effect has originated a downstream displacement of acid mixing processes affecting the estuary, which is reflected in higher metal concentration in sediments of the outer zones of the systemen_US
dc.identifier.urihttp://hdl.handle.net/10272/8868
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherGeochemistryen_US
dc.subject.otherEnrichment factoren_US
dc.subject.otherHolocene sedimentsen_US
dc.subject.otherTinto estuaryen_US
dc.subject.otherSpainen_US
dc.titleFactores de enriquecimiento metálico en sedimentos holocenos del estuario del río Tinto (SO de España)en_US
dc.titleMetal Enrichment Factors in Holocene Sediments in the Tinto River Estuary (SW Spain)eng
dc.typejournal articleen_US
dspace.entity.typePublication
relation.isAuthorOfPublicationcb4b5183-92b7-4daf-b70f-4487e49e9d97
relation.isAuthorOfPublication587516a5-d44d-41f5-9daa-d466b1fd7731
relation.isAuthorOfPublication482871a0-f9b0-490a-9264-1a031581e17c
relation.isAuthorOfPublication.latestForDiscoverycb4b5183-92b7-4daf-b70f-4487e49e9d97

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