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Iron oxide - clay composite vectors on long-distance transport of arsenic and toxic metals in mining-affected areas

AutorGómez-González, Miguel A.; Villalobos, Mario; Marco, J.F. ; García-Guinea, Javier ; Bolea, Eduardo; Laborda, Francisco; Garrido, Fernando
Palabras claveArsenic
Colloids
XAS
AF4-ICP-MS
Mine residues
Fe-coatings
Fecha de publicaciónabr-2018
EditorElsevier
CitaciónChemosphere 197: 759-767 (2018)
ResumenMine wastes from abandoned exploitations are sources of high concentrations of hazardous metal(oid)s. Although these contaminants can be attenuated by sorbing to secondary minerals, in this work we identified a mechanism for long-distance dispersion of arsenic and metals through their association to mobile colloids. We characterize the colloids and their sorbed contaminants using spectrometric and physicochemical fractionation techniques. Mechanical action through erosion may release and transport high concentrations of colloid-associated metal(oid)s towards nearby stream waters, promoting their dispersion from the contamination source. Poorly crystalline ferrihydrite acts as the principal As-sorbing mineral, but in this study we find that this nanomineral does not mobilize As independently, rather, it is transported as surface coatings bound to mineral particles, perhaps through electrostatic biding interactions due to opposing surface charges at acidic to circumneutral pH values. This association is very stable and effective in carrying along metal(oid)s in concentrations above regulatory levels. The unlimited source of toxic elements in mine residues causes ongoing, decades-long mobilization of toxic elements into stream waters. The ferrihydrite-clay colloidal composites and their high mobility limit the attenuating role that iron oxides alone show through adsorption of metal(oid)s and their immobilization in situ. This may have important implications for the potential bioavailability of these contaminants, as well as for the use of this water for human consumption.
Versión del editorhttps://doi.org/10.1016/j.chemosphere.2018.01.100
URIhttp://hdl.handle.net/10261/162000
DOI10.1016/j.chemosphere.2018.01.100
ISSN0045-6535
E-ISSN1879-1298
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