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Hydrochemical characteristics of the natural waters associated with the flooding of the Meirama open pit (A Coruñ, NW Spain)

Published online by Cambridge University Press:  05 July 2018

J. Delgado*
Affiliation:
Civil Engineering School, University of A Coruña, Campus de Elvinña s/n, 15192, A Coruña, Spain
R. Juncosa
Affiliation:
Civil Engineering School, University of A Coruña, Campus de Elvinña s/n, 15192, A Coruña, Spain
A. Vazquez
Affiliation:
Civil Engineering School, University of A Coruña, Campus de Elvinña s/n, 15192, A Coruña, Spain
I. Falcón
Affiliation:
Civil Engineering School, University of A Coruña, Campus de Elvinña s/n, 15192, A Coruña, Spain
J. Canal
Affiliation:
Civil Engineering School, University of A Coruña, Campus de Elvinña s/n, 15192, A Coruña, Spain
H. Hernández
Affiliation:
Civil Engineering School, University of A Coruña, Campus de Elvinña s/n, 15192, A Coruña, Spain
F. Padilla
Affiliation:
Civil Engineering School, University of A Coruña, Campus de Elvinña s/n, 15192, A Coruña, Spain
P. Rodríguez-Vellando
Affiliation:
Civil Engineering School, University of A Coruña, Campus de Elvinña s/n, 15192, A Coruña, Spain
J. L. Delgado
Affiliation:
Lignitos de Meirama S.A. Juana de Vega 2, 15003, A Coruña, Spain
*

Abstract

In December, 2007, after 30 years of operations, the mine of Meirama ceased extraction of brown lignite. Since then operations have begun which will lead to the formation of a big mining lake (~2 km2 surface and up to 180 m deep) after controlled flooding of the open pit. In the process of flooding, both surface and ground waters are involved, each with their own chemical signature. According to the information available, the diversion of surface waters towards the pit hole should lead to the formation of a water body of acceptable quality. However, an unassisted flooding process could eventually form an acidic lake.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2008

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References

Banks, D., Younger, P.L., Arnesen, R.T., Iversen, E.R., and Banks, S.D. (1997) Mine-water chemistry: the good, the bad and the ugly. Environmental Geology, 32, 157–174.CrossRefGoogle Scholar
Castro, J.M. and Moore, , IN. (2000) Pit lakes: their characteristics and the potential for their remediation. Environmental Geology, 39, 1254–1260.CrossRefGoogle Scholar
Graupner, B.J., Benthausb, F.C., Burger, S. and Werner, F. (2005) Implications of EU-Water Framework Directive for the East German Postmining Landscape Lausitz: Coping with a sparse knowledge of the underground. Limnologica, 35, 199–205 CrossRefGoogle Scholar
Kroll, A., Amezaga, J.M., Younger, P.L. and Wolkersdorfer, C. (2002) Regulation of Mine Waters in the European Union: Contribution of Scientific Research to Policy Development. Mine Water and the Environment, 21, 193–200.CrossRefGoogle Scholar
Nixdorf, B., Lessmann, D. and Deneke, R. (2005) Mining lakes in a disturbed landscape: Application of the EC Water Framework Directive and future management strategies. Ecological Engineering, 24, 67–73.CrossRefGoogle Scholar
Stromberg, B. and Banwart, S. (1994) Kinetic modelling of geochemical reactions at the Aitik mining waste rock site in northern Sweden. Applied Geochemistry, 9, 583–595.CrossRefGoogle Scholar
Werner, F., Bilek, F. and Luckner, L. (2001) Implications of predicted hydrologic changes on Lake Senftenberg as calculated using water and reactive mass budgets. Mine Water and the Environment, 20, 129–139.CrossRefGoogle Scholar