Transient processes associated with the flooding of the Meirama pit lake (La Coruña, Spain)

Authors

  • J. Delgado Martín E.T.S. Ingenieros de Caminos, Canales y Puertos. Universidade da Coruña
  • R. Juncosa Rivera E.T.S. Ingenieros de Caminos, Canales y Puertos. Universidade da Coruña
  • R. González Philippon Lignitos de Meirama S.A.
  • A. Fernández García Lignitos de Meirama S.A.

DOI:

https://doi.org/10.21701/bolgeomin.122.2.009

Keywords:

Brunt-Väisälä buoyancy frequency, limnology, Meirama, pit lake, Schmidt index, stability

Abstract


The Meirama pit lake is a system resulting from the currently ongoing forced flooding of an extensive gray-lignite mine. By comprehensively monitoring a wide variety of physical, chemical and biological parameters we are able to describe the main characteristics of this lake after two years of flooding. This paper focuses upon the description of the thermal structure and stability of this meromitic lake. We have been able to identify thermal and chemical homogenization processes that would have been complete after the first year of flooding but only partially so thereafter (affecting only the surface water to a depth of some 30 metres). Stability calculations support the hypothesis of partial mixing in the shallower water, where the transfer of wind energy may contribute to triggering the mixing phenomenon. The deepest waters of the lake, which are isolated by a halocline resulting from the entrance of denser waters during the firsts months of flooding, would be stable, except for the introduction of external energy, according to the results of the calculations of the Brunt-Väisäla buoyancy frequency.

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Published

2011-06-30

How to Cite

Delgado Martín, J., Juncosa Rivera, R., González Philippon, R., & Fernández García, A. (2011). Transient processes associated with the flooding of the Meirama pit lake (La Coruña, Spain). Boletín Geológico Y Minero, 122(2), 247–258. https://doi.org/10.21701/bolgeomin.122.2.009

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