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dc.creatorNieva, Nancy Eugenia-
dc.creatorBorgnino Bianchi, Laura Carolina-
dc.creatorLocati, Francisco-
dc.creatorGarcia, Maria Gabriela-
dc.date2018-05-04T19:39:42Z-
dc.date2018-05-04T19:39:42Z-
dc.date2016-04-
dc.date2018-05-02T17:41:29Z-
dc.date.accessioned2019-04-29T15:40:24Z-
dc.date.available2019-04-29T15:40:24Z-
dc.date.issued2018-05-04T19:39:42Z-
dc.date.issued2018-05-04T19:39:42Z-
dc.date.issued2016-04-
dc.date.issued2018-05-02T17:41:29Z-
dc.identifierNieva, Nancy Eugenia; Borgnino Bianchi, Laura Carolina; Locati, Francisco; Garcia, Maria Gabriela; Mineralogical control on arsenic release during sediment water interaction in abandoned mine wastes from the Argentina Puna.; Elsevier Science; The Science Of Total Environment; 550; 4-2016; 1141-1151-
dc.identifier0048-9697-
dc.identifierhttp://hdl.handle.net/11336/44220-
dc.identifierCONICET Digital-
dc.identifierCONICET-
dc.identifier.urihttp://rodna.bn.gov.ar:8080/jspui/handle/bnmm/299143-
dc.descriptionThe sulfide-rich residues of La Concordia mine, Argentina Puna, are accumulated in tailing dams that remainedexposed to the weathering agents for almost 30 years. In such period of time, a complex sequence of redoxand dissolution/precipitation reactions occurred, leading to the gradual oxidation of the wastes and the formationof weathering profiles. The sources of arsenic in the wastes were analyzed by XRD and SEM/EDS analysiswhile a standardized sequential extraction procedure was followed to define solid As associations. In addition,the release of As during sediment?water interaction was analyzed in a period of 10 months. The results indicatethat primary As-bearing minerals are arsenian pyrite and polymetallic sulfides. As-jarosite and scarce arsenatesare the only secondary As-bearing minerals identified by XRD and SEM/EDS. However, the rapid release(i.e., b1 h) of arsenic from suspensions of the studied sediments in water, seems to be associated to the dissolutionof highly soluble (hydrous)sulfates, as it was determined in samples of the efflorescences that cover the entiresite. Contributions from the more abundant As-jarosite are also expected in longer periods of sediment?water interaction, due to its low rate of dissolution in acid and oxic conditions. Finally, near 30% of As remains adsorbed onto Fe (hydr)oxides thus representing a hazardous reservoir with the potential of mobilizing As intoporewaters and streamwaters if the acidic and oxidizing conditions that predominate in the region are altered.-
dc.descriptionFil: Nieva, Nancy Eugenia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina-
dc.descriptionFil: Borgnino Bianchi, Laura Carolina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina-
dc.descriptionFil: Locati, Francisco. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina-
dc.descriptionFil: Garcia, Maria Gabriela. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina-
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dc.languageeng-
dc.publisherElsevier Science-
dc.relationinfo:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0048969716301462?via%3Dihub-
dc.relationinfo:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1016/j.scitotenv.2016.01.147-
dc.rightsinfo:eu-repo/semantics/restrictedAccess-
dc.rightshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/-
dc.sourcereponame:CONICET Digital (CONICET)-
dc.sourceinstname:Consejo Nacional de Investigaciones Científicas y Técnicas-
dc.sourceinstacron:CONICET-
dc.subjectCONCORDIA MINE-
dc.subjectCENTRAL ANDES-
dc.subjectAS-JAROSITE-
dc.subjectSCORODITE-
dc.subjectMeteorología y Ciencias Atmosféricas-
dc.subjectCiencias de la Tierra y relacionadas con el Medio Ambiente-
dc.subjectCIENCIAS NATURALES Y EXACTAS-
dc.titleMineralogical control on arsenic release during sediment water interaction in abandoned mine wastes from the Argentina Puna.-
dc.typeinfo:eu-repo/semantics/article-
dc.typeinfo:eu-repo/semantics/publishedVersion-
dc.typeinfo:ar-repo/semantics/articulo-
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