Geochemical and Limnological Characterization of the Corta Atalaya Pit Lake (Riotinto Mines, Spain)

This study examines some relevant limnological and hydrogeochemical characteristics of the most emblematic pit lake of the Iberian Pyrite Belt (IPB). Corta Atalaya (CA) open pit mine is known for its large size and for being one of the most important exploitations of copper in Europe. Despite its hi...

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Main Authors: Esther Santofimia, Blanca Rincón-Tomás, Enrique López-Pamo, Francisco Javier González, Ricardo Amils
Format: Article
Language:English
Published: MDPI AG 2023-12-01
Series:Materials Proceedings
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Online Access:https://www.mdpi.com/2673-4605/15/1/66
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author Esther Santofimia
Blanca Rincón-Tomás
Enrique López-Pamo
Francisco Javier González
Ricardo Amils
author_facet Esther Santofimia
Blanca Rincón-Tomás
Enrique López-Pamo
Francisco Javier González
Ricardo Amils
author_sort Esther Santofimia
collection DOAJ
description This study examines some relevant limnological and hydrogeochemical characteristics of the most emblematic pit lake of the Iberian Pyrite Belt (IPB). Corta Atalaya (CA) open pit mine is known for its large size and for being one of the most important exploitations of copper in Europe. Despite its historical importance, little is known about the lake formed in this open pit. During this study, the pit lake presented a surface area of 16 ha, a maximum depth of 106 m, and a 5.8 hm<sup>3</sup> volume of acid and metal-enriched water. CA pit lake shows permanent chemical stratification (meromictic lake), where three layers with different density and chemical composition can be differentiated: (i) a superficial layer of 5 ± 2 m water depth, with electric conductivity (EC) between 5.4–6.64 mS/cm, and oxygenated and Fe(III)-rich mixolimnion; (ii) an intermediate layer (between 5–30 m, chemocline), exhibiting strong vertical changes in parameters such as temperature (T) and EC, which show an increase with depth; and (iii) a thick bottom layer from 30 m to 106 m depth, with anoxic, elevated EC (47 mS/cm) and T (32 °C) values, and a concentration of Fe as Fe(II) (monimolimnion).The characterization of the water column is essential to know the potential sources of strategic and critical raw materials, and to evaluate their possible recuperation, thereby activating a circular economy.
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spelling doaj-art-8356aef17c2d4439824b79b089fef8eb2025-08-20T02:21:13ZengMDPI AGMaterials Proceedings2673-46052023-12-011516610.3390/materproc2023015066Geochemical and Limnological Characterization of the Corta Atalaya Pit Lake (Riotinto Mines, Spain)Esther Santofimia0Blanca Rincón-Tomás1Enrique López-Pamo2Francisco Javier González3Ricardo Amils4Geological Survey of Spain, Spanish National Research Council (IGME-CSIC) Ríos Rosas 23, 28003 Madrid, SpainGeological Survey of Spain, Spanish National Research Council (IGME-CSIC) Ríos Rosas 23, 28003 Madrid, SpainGeological Survey of Spain, Spanish National Research Council (IGME-CSIC) Ríos Rosas 23, 28003 Madrid, SpainGeological Survey of Spain, Spanish National Research Council (IGME-CSIC) Ríos Rosas 23, 28003 Madrid, SpainCentro de Biología Molecular Severo Ochoa (CSIC-UAM), Universidad Autónoma de Madrid, Campus Cantoblanco, 28049 Madrid, SpainThis study examines some relevant limnological and hydrogeochemical characteristics of the most emblematic pit lake of the Iberian Pyrite Belt (IPB). Corta Atalaya (CA) open pit mine is known for its large size and for being one of the most important exploitations of copper in Europe. Despite its historical importance, little is known about the lake formed in this open pit. During this study, the pit lake presented a surface area of 16 ha, a maximum depth of 106 m, and a 5.8 hm<sup>3</sup> volume of acid and metal-enriched water. CA pit lake shows permanent chemical stratification (meromictic lake), where three layers with different density and chemical composition can be differentiated: (i) a superficial layer of 5 ± 2 m water depth, with electric conductivity (EC) between 5.4–6.64 mS/cm, and oxygenated and Fe(III)-rich mixolimnion; (ii) an intermediate layer (between 5–30 m, chemocline), exhibiting strong vertical changes in parameters such as temperature (T) and EC, which show an increase with depth; and (iii) a thick bottom layer from 30 m to 106 m depth, with anoxic, elevated EC (47 mS/cm) and T (32 °C) values, and a concentration of Fe as Fe(II) (monimolimnion).The characterization of the water column is essential to know the potential sources of strategic and critical raw materials, and to evaluate their possible recuperation, thereby activating a circular economy.https://www.mdpi.com/2673-4605/15/1/66acid pit lakeIberian Pyrite Beltraw materialsheavy metalslimnology
spellingShingle Esther Santofimia
Blanca Rincón-Tomás
Enrique López-Pamo
Francisco Javier González
Ricardo Amils
Geochemical and Limnological Characterization of the Corta Atalaya Pit Lake (Riotinto Mines, Spain)
Materials Proceedings
acid pit lake
Iberian Pyrite Belt
raw materials
heavy metals
limnology
title Geochemical and Limnological Characterization of the Corta Atalaya Pit Lake (Riotinto Mines, Spain)
title_full Geochemical and Limnological Characterization of the Corta Atalaya Pit Lake (Riotinto Mines, Spain)
title_fullStr Geochemical and Limnological Characterization of the Corta Atalaya Pit Lake (Riotinto Mines, Spain)
title_full_unstemmed Geochemical and Limnological Characterization of the Corta Atalaya Pit Lake (Riotinto Mines, Spain)
title_short Geochemical and Limnological Characterization of the Corta Atalaya Pit Lake (Riotinto Mines, Spain)
title_sort geochemical and limnological characterization of the corta atalaya pit lake riotinto mines spain
topic acid pit lake
Iberian Pyrite Belt
raw materials
heavy metals
limnology
url https://www.mdpi.com/2673-4605/15/1/66
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