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The Positive Environmental Contribution of Jarosite by Retaining Lead in Acid Mine Drainage Areas

Jarosite, KFe(3)(SO(4))(2)(OH)(6), is a secondary iron sulphate often found in acid mine drainage (AMD) environments, particularly in mining wastes from polymetallic sulphide ore deposits. Despite the negative environmental connotation usually ascribed to secondary sulphate minerals due to the relea...

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Detalles Bibliográficos
Autores principales: Figueiredo, Maria-Ondina, da Silva, Teresa Pereira
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Molecular Diversity Preservation International (MDPI) 2011
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3108128/
https://www.ncbi.nlm.nih.gov/pubmed/21655138
http://dx.doi.org/10.3390/ijerph8051575
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author Figueiredo, Maria-Ondina
da Silva, Teresa Pereira
author_facet Figueiredo, Maria-Ondina
da Silva, Teresa Pereira
author_sort Figueiredo, Maria-Ondina
collection PubMed
description Jarosite, KFe(3)(SO(4))(2)(OH)(6), is a secondary iron sulphate often found in acid mine drainage (AMD) environments, particularly in mining wastes from polymetallic sulphide ore deposits. Despite the negative environmental connotation usually ascribed to secondary sulphate minerals due to the release of hazardous elements to aquifers and soils, jarosite acts as an efficient remover and immobilizer of such metals, particularly lead. The mineral chemistry of jarosite is reviewed and the results of a Fe K-edge XANES (X-Ray Absorption Near-Edge Structure) study of K-, Na- and Pb-jarosite are described and discussed within the context of the abandoned old mines of São Domingos and Aljustrel located in southern Portugal, in the Iberian Pyrite Belt (IPB).
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spelling pubmed-31081282011-06-08 The Positive Environmental Contribution of Jarosite by Retaining Lead in Acid Mine Drainage Areas Figueiredo, Maria-Ondina da Silva, Teresa Pereira Int J Environ Res Public Health Article Jarosite, KFe(3)(SO(4))(2)(OH)(6), is a secondary iron sulphate often found in acid mine drainage (AMD) environments, particularly in mining wastes from polymetallic sulphide ore deposits. Despite the negative environmental connotation usually ascribed to secondary sulphate minerals due to the release of hazardous elements to aquifers and soils, jarosite acts as an efficient remover and immobilizer of such metals, particularly lead. The mineral chemistry of jarosite is reviewed and the results of a Fe K-edge XANES (X-Ray Absorption Near-Edge Structure) study of K-, Na- and Pb-jarosite are described and discussed within the context of the abandoned old mines of São Domingos and Aljustrel located in southern Portugal, in the Iberian Pyrite Belt (IPB). Molecular Diversity Preservation International (MDPI) 2011-05 2011-05-13 /pmc/articles/PMC3108128/ /pubmed/21655138 http://dx.doi.org/10.3390/ijerph8051575 Text en © 2011 by the authors; licensee MDPI, Basel, Switzerland. http://creativecommons.org/licenses/by/3.0 This article is an open-access article distributed under the terms and conditions of the Creative Commons Attribution license (http://creativecommons.org/licenses/by/3.0/).
spellingShingle Article
Figueiredo, Maria-Ondina
da Silva, Teresa Pereira
The Positive Environmental Contribution of Jarosite by Retaining Lead in Acid Mine Drainage Areas
title The Positive Environmental Contribution of Jarosite by Retaining Lead in Acid Mine Drainage Areas
title_full The Positive Environmental Contribution of Jarosite by Retaining Lead in Acid Mine Drainage Areas
title_fullStr The Positive Environmental Contribution of Jarosite by Retaining Lead in Acid Mine Drainage Areas
title_full_unstemmed The Positive Environmental Contribution of Jarosite by Retaining Lead in Acid Mine Drainage Areas
title_short The Positive Environmental Contribution of Jarosite by Retaining Lead in Acid Mine Drainage Areas
title_sort positive environmental contribution of jarosite by retaining lead in acid mine drainage areas
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3108128/
https://www.ncbi.nlm.nih.gov/pubmed/21655138
http://dx.doi.org/10.3390/ijerph8051575
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