Acid Mine Drainage: A Huge Problem Around Abandoned Mines

Acid mine drainage (AMD) is an acidic mineral solution that flows out of a mine. The phenomenon in question is spontaneous and involves metal sulfides (type “M” Sx) with no economic value in mining. Indeed, during mining work (excavations and pumping), the chemical balance of these outcrops and deep deposits are disturbed by sudden changes in oxidation-reduction conditions. This reaction is of sufficient magnitude to cause large flows.

The oxidation of pyrite (FeS2) plays a central role in the production of acid mine drainage. This mineral represents most of the sulfide phases. This oxidation is governed by a set of reactions and takes place in three phases. The first step is the oxidation of pyrite by oxygen in the aqueous phase: the sulfur is then oxidized to sulfate (SO42-), and the iron is solubilized in the form of ferrous Fe2+ ions:


FeS2 + 7/2 O2 + H2O ⇌ 2 SO42- + Fe2+ + 2 H+

Step 2 is the oxidation of ferrous ions to ferric ions (Fe3+) by dissolved oxygen:

Fe2+ + ¼ O2 + H+ ⇌ Fe3+ + ½ H2O


This step does not affect the pyrite, but is a prerequisite in step 3, in which the oxidation no longer requires the action of oxygen since it is the aqueous oxidation of pyrite (in sulfate) by ferric ions (Fe3+):

FeS2 + 14 Fe3+ + 8 H2O ⇌ 2 SO42- + 15 Fe2+ + 16 H+

As I already wrote in my previous article, AMD from mine waste and contaminations of soils and water with metals are considered as major environmental problems in mining areas. Consequently, acidification would increase the dissolution of toxic metals from tailings, waste rock piles, and open pits. Therefore, soil and water ecosystems will be contaminated. Certainly, as rainwater infiltrates the underground soil/rock, it can cause pore-water flow in the pore space of the soil/rock. The resulting pore-water flow can react chemically with the mine waste, dissolving metals at the mine site. Since the dissolved metals can be transported in the soil/rock through pore-water reactions, they can contaminate both the land and the groundwater at the mine site.

In a study conducted with colleagues from the University of Marrakech (Morocco), we have analyzed the impact of mining activity on the surrounding soils around the abandoned of Kettara mine (Morocco).

The objectives of this study were to (i) characterize soils and tailings; (ii) determine the geochemical background of chemical elements in soils of the region; and (iii) propose geochemical maps regarding the selected elements. Indeed, one of the most serious environmental issues related to the mining industry in Morocco and around the world is pollution from abandoned mine sites. Mine waste is an obvious source of soil contamination. Climatic effects such as heavy rainfall engender metal dispersion in semi-arid areas since soils are typically scarcely vegetated. In this study, we assessed the extension and magnitude of soil contaminations with toxic elements from abandoned Kettara mine in Morocco, using geochemical analysis and geostatistics for mapping. Soils and mine waste were sampled and analyzed for 41 chemical elements. Based on the enrichment factor, only four metals and one metalloid of interest (Cu, Pb, Zn, As, and Fe) were selected in this research. A geochemical background was determined using exploratory data analysis, and geochemical maps were elaborated using geostatistics in a Geographic Information System environment.

Photograph of tailings around the Kettara site. Credit: Olivier POURRET
Geochemical map of copper distribution around the Kettara mine (red color express high values whereas blue color expresses low concentration. Credit: Olivier POURRET

The obtained results showed that Kettara soils are contaminated with metals and metalloids that exceed the established geochemical background values (Cu≈43.8 mg/kg, Pb≈21.8 mg/kg, Zn≈102.6 mg/kg, As≈13.9 mg/kg and Fe≈56,978 mg/kg). Geochemical maps showed that the deposited mine wastes are responsible for soil contamination, with released metals and metalloid that have been dispersed downstream from the mine waste, mainly through water after rainfall. The comparison of these findings with the geochemical background reveals the degree of pollution of the Kettara mine site’s surrounding soils and raises the question of possible health risks.

Photograph of the Kettara village near the abandoned mine. Credit: Olivier POURRET

For sustainable development and environmental planning, the current study will serve as a reference for politicians, managers, and decision-makers to assess soil contamination in abandoned mine sites in Morocco.

These findings are described in the article entitled Assessment of soil contamination around an abandoned mine in a semi-arid environment using geochemistry and geostatistics: Pre-work of geochemical process modeling with numerical models, published in the Journal of Geochemical Exploration.

Further studies on the pollution of the groundwater were performed by my colleague from UniLaSalle, Lahcen Zouhri (Moyé et al. 2017).


  1. Khalil, A., Hanich, L., Bannari, A., Zouhri, L., Pourret, O., Hakkou, R., 2013. Assessment of soil contamination around an abandoned mine in a semi-arid environment using geochemistry and geostatistics: Pre-work of geochemical process modeling with numerical models. Journal of Geochemical Exploration, 125: 117-129.
  2. Moyé, J., Picard-Lesteven, T., Zouhri, L., El Amari, K., Hibti, M., Benkaddour, A., 2017. Groundwater assessment and environmental impact in the abandoned mine of Kettara (Morocco). Environmental Pollution, 231(Part 1): 899-907.

About The Author

Olivier Pourret received his PhD in Earth Sciences in 2006 from Université de Rennes 1 (France). He is now an associate professor of geochemistry at UniLaSalle, Beauvais (France) and co-head of the research group AGHYLE (Agroecology and Hydrogeochemistry). In 2013, Olivier Pourret received his Habilitation in Earth Sciences from Université Picardie Jules Verne (France). He is a Fellow member of the Society of Economic Geologists and member of the Geochemical Society, European Association of Geochemistry, American Geophysical Union and American Chemical Society. His research interests include trace metal fractionation and particularly critical elements (rare earth elements, cobalt, vanadium) in low-temperature aqueous systems, a better understanding of trace metal cycles in natural waters, and an improved knowledge of trace metals mobility from rock to soils and vegetation in the critical zone.