The acidic mine pit lakes of the Iberian Pyrite Belt: An approach to their physical limnology and hydrogeochemistry

2008 ◽  
Vol 23 (5) ◽  
pp. 1260-1287 ◽  
Author(s):  
Javier Sánchez España ◽  
Enrique López Pamo ◽  
Esther Santofimia Pastor ◽  
Marta Diez Ercilla
2009 ◽  
Vol 28 (1) ◽  
pp. 15-29 ◽  
Author(s):  
Javier Sánchez España ◽  
Enrique López Pamo ◽  
Marta Diez ◽  
Esther Santofimia

PLoS ONE ◽  
2013 ◽  
Vol 8 (6) ◽  
pp. e66746 ◽  
Author(s):  
Esther Santofimia ◽  
Elena González-Toril ◽  
Enrique López-Pamo ◽  
María Gomariz ◽  
Ricardo Amils ◽  
...  

2013 ◽  
Vol 825 ◽  
pp. 23-27 ◽  
Author(s):  
Elena González-Toril ◽  
Esther Santofimia ◽  
Enrique López-Pamo ◽  
Enoma O. Omoregie ◽  
Ricardo Amils ◽  
...  

Abstract. In mining areas in which sulfur-containing ores are exposed, the oxidation of sulfides leads to the formation of acidic mine drainage (AMD) waters. Both traditional and molecular microbial studies have shown that chemolithotrophic sulfur- and iron-oxidizing bacteria are responsible for this activity. The Iberian Pyrite Belt (IPB), located in southwestern Spain represents one of the world’s largest accumulations of mine wastes and AMD waters. Mineralogical and textural characteristics of the IPB ores favor the oxidation and dissolution of pyrite and the subsequent formation of AMD waters. Acidic pit lakes in the IPB are a hotspot for this activity. These pit lakes are former open pit mines where ores have been exposed leading the formation of AMD waters. At present, there are more than 25 of these pit lakes between the provinces of Huelva and Seville (SW Spain). This work reports the physical properties, hydrogeochemical characteristics, and microbial diversity of two pit lakes located in the IPB Nuestra Señora del Carmen (NSC), and Concepción (CN). Both pit lakes are acid (pH 2-4) and showed chemical and thermal stratification with well defined chemoclines. One particular characteristic of NSC is that it has developed a chemocline very close to the surface (2 m depth). Microbial community composition of the water column was analyzed by 16S and 18S rRNA gene cloning and sequencing. The microorganisms detected in NSC are characteristic of acid mine drainage (AMD), including iron oxidizing bacteria (Leptospirillum) and facultative iron reducing bacteria and archaea (Acidithiobacillus ferrooxidans, Actinobacteria, Acidimicrobiales, Ferroplasma) detected in the bottom layer. Diversity in CN was higher than in NSC. Microorganisms known from AMD systems (Acidiphilium, Acidobacteria and Ferrovum) and microorganisms never reported from AMD systems were both identified.


2013 ◽  
Vol 825 ◽  
pp. 19-22 ◽  
Author(s):  
Carmen Falagán ◽  
F.J. Sánchez-España ◽  
D. Barrie Johnson

The microbiology and geochemistry of two pit lakes at former metal mines (Cueva de la Mora and Guadiana) located in the Iberian Pyrite Belt in Spain were investigated. Both lakes are meromictic, with more acidic and oxidized mixolimnion zones overlying anoxic monimolimnion zones, and transitional chemoclines with characteristic sharp pH and redox potential gradients. Stratification in the pit lakes was reflected in the size and diversity of the microbial communities in the different zones, with the chemocline of Cueva de la Mora pit lake and the hypolimnion (the lower layer of the mixolimnion) in the Guadiana pit lake containing the most complex and abundant microbial communities. Acidophiles that oxidize and reduce both iron and sulfur co-exist within the chemocline/hypolimnion zones, implying that biogeochemical cycling of these two elements is most intense within these layers of the pit lakes. Novel species of bacteria were detected using molecular techniques and, in some cases, isolated and partially characterized. The latter included a novel acidophilic iron-reducing gammaproteobacterium (Acidibacter ferrireducens)


2019 ◽  
Vol 98 ◽  
pp. 09007
Author(s):  
Patrícia Gomes ◽  
Teresa Valente ◽  
Mayara Cordeiro ◽  
Filipa Moreno

The Iberian Pyrite Belt (IPB) is a world-class metallogenic province with volcanogenic massive sulphide ore deposits. Most ore exploitation occurred since pre-Roman time, creating extensive galleries, wells, waste-dumps and pit lakes. These last structures are a concern for their potential environmental impact because they accumulate large volumes of mine water affected acid mine drainage. The present work classifies the pit lakes based on the surface water hydrochemistry. Using the Ficklin diagram for classification, pit lake waters vary from acid, high-metal to high-acid, extreme-metal and exhibit similarities with other pit lakes from the Spanish sector of the IPB.


2018 ◽  
Vol 566 ◽  
pp. 807-817 ◽  
Author(s):  
Raúl Moreno González ◽  
Manuel Olías ◽  
Francisco Macías ◽  
Carlos Ruiz Cánovas ◽  
Rubén Fernández de Villarán

Author(s):  
Martin Schultze ◽  
Bertram Boehrer ◽  
Kurt Friese ◽  
Matthias Koschorreck ◽  
Sebastian Stasik ◽  
...  
Keyword(s):  

2019 ◽  
Author(s):  
Daniel Francis ◽  
◽  
Matthew B.J. Lindsay ◽  
Lee Barbour

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