Acid mine drainage — AQA A-Level Environmental Science
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Acid mine drainage (AMD) occurs when sulphide minerals such as iron pyrite are exposed to oxygen and water during mining, producing sulphuric acid that leaches toxic heavy metals into aquatic ecosystems. This process severely lowers water pH and mobilises bioaccumulative contaminants, requiring targeted remediation strategies such as limestone neutralisation and constructed wetlands.
Acid mine drainage explained
The acidic water of acid mine drainage dissolves and carries away metals that would otherwise stay locked in rock and sediment.
Read the full explanation
At low pH, metal ions such as Fe²⁺, Cu²⁺, Zn²⁺, Pb²⁺ and Al³⁺ become more soluble, so they leave the solid phase and enter the water as dissolved species. This increased solubility allows the metals to be mobilised, meaning they are transported downstream away from the mine site and can contaminate soils, sediments and drinking water. In a multiple-choice question, connect the low pH to greater solubility, then to mobilisation and toxic effects on organisms and water supplies. Distinguish mobilisation (movement into and through water) from simple deposition at the source.
Your focus
- Explain why low pH increases the solubility of metal ions.
- Describe how dissolved metals are mobilised away from a mine site.
- State one toxic effect of mobilised metals on ecosystems or water supplies.
Acid mine drainage exam tips
Topic Overview
Acid mine drainage (AMD) is a major chemical pollutant stream resulting from extractive industries, specifically metal ore and coal mining. When previously deep, anoxic deposits containing sulphide minerals—most notably iron pyrite (FeS2)—are fractured and exposed to water and atmospheric oxygen, chemical and biological oxidation generates dilute sulphuric acid.
This low-pH discharge leaches hazardous heavy metals from surrounding geology, creating a toxic, highly acidic effluent that causes severe, long-term degradation of freshwater aquatic habitats. Within AQA A-Level Environmental Science, this topic synthesises concepts from mineral extraction, aquatic pollution, biotic indices, and chemical/biological remediation strategies.
Key Concepts
- →Pyrite Oxidation Chemistry: 2FeS2 + 7O2 + 2H2O -> 2Fe2+ + 4SO4(2-) + 4H+. The reaction is autotrophic and heavily catalysed by extremophilic acidophilic bacteria such as Acidithiobacillus ferrooxidans.
- →Heavy Metal Mobilisation: Acidic water shifts metal equilibria, solubilising harmful cations (e.g. Al3+, Cd2+, Pb2+, Cu2+) that are normally locked within insoluble mineral matrices at neutral pH.
- →Benthic Smothering ('Yellow Boy'): As acidic effluent enters higher-pH river systems downstream, iron precipitates out as insoluble iron(III) hydroxide (Fe(OH)3), coating riverbeds in thick orange flocculant and smothering benthic biota.
- →Remediation Methods: Active treatment relies on chemical dosing (e.g. crushed limestone/slaked lime addition to raise pH), whereas passive treatment utilizes constructed anaerobic reed beds and limestone drains.
Marking Points
- Explains that low pH increases the solubility of metal ions such as Fe²⁺, Cu²⁺, Zn²⁺, Pb²⁺ and Al³⁺.
- States that increased solubility allows toxic metals to move from solid rock or sediment into the water.
- Describes mobilisation as the downstream transport of dissolved metals away from the mine site.
- Links mobilised toxic metals to contamination of water supplies, sediments and harm to organisms.
Examiner Tips
- 💡Trace the chain: low pH, then increased solubility, then mobilisation, then toxic impact.
- 💡Use correct ion notation such as Cu²⁺ and Al³⁺ when naming mobilised metals.
- 💡Reject options that describe metals remaining immobile or being removed from solution by the acid.
- 💡Always reference both physical and chemical consequences: do not just state that the water becomes acidic, explicitly explain the precipitation of ferric hydroxide ('yellow boy') and metal ion mobilisation.
- 💡Use proper chemical nomenclature when discussing remediation; distinguish between active additions (calcium carbonate, calcium hydroxide) and passive biological systems (constructed wetlands containing sulphate-reducing bacteria).
Common Mistakes
- Assumes metals stay locked in rock regardless of pH; state that low pH increases their solubility and release.
- Confuses mobilisation with deposition at the source; describe mobilisation as transport of dissolved metals away from the site.
- Names only one metal as the sole toxic species; recognise that several metal ions become more soluble at low pH.
- Misconception: Acid mine drainage only occurs while a mine is actively working. Correction: AMD is frequently worse in abandoned, flooded underground mines where unmanaged spoil heaps and exposed adits continuously leach acid for decades or centuries after operations cease.
- Misconception: Crushed limestone completely cleans AMD effluents. Correction: While limestone neutralises sulphuric acid and raises pH, toxic heavy metal precipitates remain as contaminated sludge that must be physically settled, filtered, and safely disposed of.
Revision Plan
- 1Step 1: Memorise the reactants and conditions of pyrite oxidation, including the bacterial action of Acidithiobacillus ferrooxidans.
- 2Step 2: Diagram the chain of ecological effects: low pH -> metal mobilisation -> gill damage -> benthic sedimentation ('yellow boy') -> loss of sensitive macroinvertebrates.
- 3Step 3: Compare and contrast active remediation (limestone dosing) vs passive remediation (wetlands, anoxic limestone drains) in terms of cost, maintenance, and long-term viability.
- 4Step 4: Practice quantitative exam questions involving water treatment volumes, neutralization stoichiometries, and interpretation of biotic index data.
Exam Question Types
- 📋Short chemical explanations (2-3 marks): Outlining how pyrite exposure and bacterial catalysts form sulphuric acid.
- 📋Ecological impact evaluations (4-6 marks): Assessing the trophic impacts of low pH, metal toxicity, and ferric hydroxide deposits on stream communities.
- 📋Remediation comparison questions (6-9 marks): Evaluating active chemical treatment versus passive constructed wetland strategies.
Command Word Expectations (AQA)
Give clear scientific reasons and mechanisms showing cause and effect (e.g. explain how bacterial oxidation of pyrite leads to aquatic biodiversity decline).
Weigh up advantages, disadvantages, costs, and environmental efficacy of specific methods (e.g. active chemical dosing vs passive reed beds), culminating in a reasoned concluding judgment.
How Students Lose Marks (Examiner Pitfalls)
Step-by-Step Worked Solutions
Question: A disused copper mine discharges drainage water at a rate of 40 m3 per hour with a sulphuric acid concentration of 0.05 mol dm-3. Calculate the mass of pure calcium carbonate (CaCO3) in kilograms required per 24-hour day to neutralise this drainage completely. (Molar mass of CaCO3 = 100.1 g mol-1; 1 mole of CaCO3 neutralises 1 mole of H2SO4).
- 1.Step 1: Calculate total volume of drainage per day: Volume = 40 m3/hour * 24 hours = 960 m3. Convert to dm3: 960 * 1,000 = 960,000 dm3.
- 2.Step 2: Calculate moles of sulphuric acid produced per day: Moles = Concentration * Volume = 0.05 mol dm-3 * 960,000 dm3 = 48,000 moles of H2SO4.
- 3.Step 3: Determine mass of CaCO3 required using stoichiometric ratio 1:1: Moles of CaCO3 = 48,000 moles. Mass in grams = 48,000 mol * 100.1 g mol-1 = 4,804,800 g.
- 4.Step 4: Convert grams to kilograms: 4,804,800 / 1,000 = 4,804.8 kg.
Question: Explain the ecological mechanisms by which acid mine drainage reduces biodiversity in a lotic freshwater ecosystem. [6 marks]
- 1.Step 1: Explain the primary chemical change: the release of sulphuric acid drastically lowers the pH of the stream water below tolerance thresholds for stenohaline/sensitive taxa (e.g. mayfly nymphs).
- 2.Step 2: Explain metal mobilisation: low pH increases the solubility of heavy metals (e.g. aluminium, copper, zinc), converting them into toxic, bioavailable free metal ions.
- 3.Step 3: Detail physical and physiological effects on fish: aluminium hydroxide precipitates over gill filaments, causing excessive mucus production, respiratory failure, and impaired osmoregulation.
- 4.Step 4: Describe habitat degradation: dissolved iron oxidises and precipitates as ferric hydroxide ('yellow boy'), coating gravel substrates, suffocating benthic invertebrates, and smothering fish spawning gravels.
- 5.Step 5: Detail food web disruption: the loss of primary producers (macrophytes, sensitive algae) and benthic detritivores collapses trophic energy transfer, reducing species richness across trophic guilds.