1. Aerobic wetlands
These shallow, vegetation-rich wetlands are designed to oxidize and remove metals, mainly iron and manganese, from slightly acidic to alkaline mine drainage water. Ferrous iron (Fe²⁺) oxidizes to ferric iron (Fe³⁺) in the presence of atmospheric oxygen, forming ferric hydroxide (Fe(OH)₃) through hydrolysis. Manganese requires a higher pH, typically above 8, to precipitate. However, aerobic wetlands are most effective when paired with pretreatment systems that ensure water alkalinity. These wetlands are also suitable for refining and improving water quality.
2. Anaerobic wetlands
These wetlands combine organic matter with limestone to create conditions that favour sulfate-reducing bacteria, which increase alkalinity. These sulfate-reducing bacteria convert sulfates into hydrogen sulfide, which reacts with dissolved metals to form stable metal sulfides. Limestone raises pH levels and provides bicarbonate alkalinity. However, the efficiency of anaerobic wetlands depends on the quality of their organic matter and limestone. Over time, precipitate buildup can clog the system, reducing performance.
3. Anoxic limestone drains
Anoxic limestone drains are buried limestone channels that prevent oxygen from entering, reducing the risk of clogging from iron hydroxides. Acidic water flows through the limestone, dissolving calcium carbonate, which neutralizes acidity and increases alkalinity. These drains are less effective for AMD with high aluminum concentrations, as aluminum can cause clogging. They are best suited for AMD from coal mines, which generally exhibit lower acidity and iron levels.
4. Vertical-flow wetlands
This system mixes organic materials and limestone in a layered, vertical flow design. The water flows through the organic layer, where oxygen is removed, and then flows through limestone, which raises the alkalinity. These systems are effective for treating highly acidic mine drainage but require regular maintenance to clear metal precipitates.
5. Open limestone channels and limestone leaching beds
These systems route AMD across or through limestone to neutralize acidity by raising pH levels, allowing metals to deposit as hydroxides. However, these open limestone channels are prone to clogging, as precipitates coat the limestone, diminishing long-term effectiveness.
6. Permeable reactive barriers
Permeable reactive barriers are underground barriers filled with reactive materials such as limestone or organic matter. These barriers intercept AMD, raising alkalinity and causing metals to deposit as sulfides or hydroxides. They work well for onsite treatment, particularly in remote or cold areas. However, their effectiveness can decline over time as precipitates fill up the reactive spaces.