Pb–Zn–Cd–As Pollution in Soils Affected 1 by Mining Activities in Central and Southern 2 Spain: a Scattered Legacy Posing Potential 3 Environmental and Health Concerns

In this chapter, published geochemical data for soils from several Pb–Zn mine sites and districts from Spain are reviewed. Although most of the mines have closed down, a legacy of highly polluted soils still remains throughout the sites constituting a potential hazard for the environment and human h...

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Detalles Bibliográficos
Autores: Lillo, Javier, Oyarzun Muñoz, Roberto, Esbrí Víctor, José María, García Lorenzo, María de la Luz, Higueras, Pablo
Tipo de recurso: capítulo de libro
Fecha de publicación:2015
País:España
Institución:Universidad Complutense de Madrid (UCM)
Repositorio:Docta Complutense
Idioma:inglés
OAI Identifier:oai:docta.ucm.es:20.500.14352/35811
Acceso en línea:https://hdl.handle.net/20.500.14352/35811
Access Level:acceso abierto
Palabra clave:550.4(460)
(460)550.4
631.41(460)
(460)631.41
Arsenic
Environmental geochemistry
Iberian Peninsula
Metals
Mine sites
Soils
Arsénico
Geoquímica
Península Ibérica
Metales
Minas
Suelos
2503 Geoquímica
Descripción
Sumario:In this chapter, published geochemical data for soils from several Pb–Zn mine sites and districts from Spain are reviewed. Although most of the mines have closed down, a legacy of highly polluted soils still remains throughout the sites constituting a potential hazard for the environment and human health. The fate of the studied metals and metalloids in these soils is mainly controlled by factors such as mining methods, concentration and metallurgical operations, mineralogy of the ore, gangue and host rock, fracturing of the host rocks, physiography, climate, and soil types (pedogenic evolution). It can be concluded that the most polluted soils (identified on the basis of an enrichment factor) are those of the Sierra Minera (La Unión District – SE Spain), at more than 488 (Pb), 163 (Zn), 99 (Cd), and 1698 (As) times the background values from non-contaminated soils. Pb is usually related to As, which in turn is bound to Fe oxides and oxyhydroxides.Metal bearing jarosite and other soluble phases also play a relevant role in the studied soil–water systems, because these minerals are dissolved during intense rainy events, thus resulting in high rates of metal leaching and mobilization by runoff.