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dc.contributor.authorFernández Caliani, Juan Carlos 
dc.contributor.authorTimón, V.
dc.contributor.authorRivera Cantero, María Belén
dc.contributor.authorGiráldez Díaz, Inmaculada 
dc.contributor.authorPérez López, Rafael 
dc.date.accessioned2018-07-12T07:39:57Z
dc.date.available2018-07-12T07:39:57Z
dc.date.issued2013
dc.identifier.citationFernández Caliani, J.C., Timón, V., Rivera Cantero, M.B., Giráldez Díaz, I., Pérez López, R. (2013). Experimental and theoretical evidence of zinc structurally bound in vermiculite from naturally metal-enriched soils. Clay Minerals, 48(3), 529-541. https://doi.org/10.1180/claymin.2013.048.3.09es_ES
dc.identifier.issn0009-8558
dc.identifier.issn1471-8030 (electrónico)
dc.identifier.urihttp://hdl.handle.net/10272/15053
dc.description.abstractThis paper provides evidence of appreciable amounts of Zn (up to 0.52 a.p.f.u.) residing in the crystal structure of trioctahedral vermiculite; the results were obtained by a combination of experimental methods (X-ray diffraction, energy dispersive X-ray spectrometry, electron microprobe analysis and selective chemical extractions) and theoretical studies based on density functional theory (DFT). Vermiculite occurs in size fractions ranging from 10 to 40 mm of near-neutral soils naturally enriched in Zn (up to 8110 mg kg 1) due to the weathering of carbonatehosted Zn-Pb deposits in SW Spain. Zinc was partitioned among the various pedogenic phases during soil formation, but the larger part (>80%) was concentrated in the residual silicate fraction. The soil exchangeable Zn pool was found to be virtually negligible. The DFT calculations support the hypothesis that the role of vermiculite is an effective sink for geogenic Zn; this is consistent, in terms of energetic stability, with the assumption that most Zn is structurally bound in octahedral sheets rather than in the interlayer exchange sites. The findings conclusively indicate that the potential mobility of Zn should remain low under the present soil conditions.es_ES
dc.language.isoenges_ES
dc.publisherMineralogical Societyes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherZinces_ES
dc.subject.otherVermiculitees_ES
dc.subject.otherSoiles_ES
dc.subject.otherGeogenic enrichmentes_ES
dc.subject.otherMetal partitioninges_ES
dc.subject.otherSelective chemical extractionses_ES
dc.subject.otherDensity functional theoryes_ES
dc.titleExperimental and theoretical evidence of zinc structurally bound in vermiculite from naturally metal-enriched soilses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherversionhttps://doi.org/10.1180/claymin.2013.048.3.09es_ES
dc.identifier.doi10.1180/claymin.2013.048.3.09
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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