11.6
Mining exposes pyrite to oxygen in the air and water from rain or groundwater, initiating a series of oxidation reactions that release ferrous iron.
This reaction also produces sulfuric acid, which leaches into the surrounding ecosystems and damages them.
Certain acid-loving bacteria grow well on mine rocks and speed up the pyrite oxidation.
For example, Acidithiobacillus ferrooxidans and Leptospirillum ferrooxidans oxidize the ferrous iron into ferric iron.
The resulting ferric iron then accelerates the oxidation of more pyrite, creating a self-sustaining cycle that continues to generate sulfuric acid.
As the acidic runoff flows into oxygen-rich streams, more ferrous iron is oxidized into ferric iron.
Ferric iron reacts with water to form insoluble iron hydroxide, often seen as an orange or reddish sludge.
When this acidic water reaches rivers, it further dissolves toxic metals, such as aluminum and cadmium, harming aquatic life.
Mining activities that disturb sulfide-rich rocks, particularly those containing pyrite (FeS₂), initiate a cascade of geochemical and microbiological…
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