Surface mining may impair groundwater in numerous ways: by drainage of usable water from shallow aquifers; lowering of water levels in adjacent areas and changes in flow direction within aquifers; contamination of usable aquifers below mining operations due to infiltration (percolation) of poor-quality
mine water; and increased infiltration of precipitation on spoil piles. Where coal or carbonaceous shale is present, increased infiltration may result in: increased runoff of poor-quality water and erosion from spoil piles, recharge of poor-quality water to shallow groundwater aquifers and poor-quality water flow to nearby streams. The contamination of both groundwater and nearby streams may be for long periods of time. Deterioration of stream quality results from
acid mine drainage, toxic trace elements, high content of dissolved solids in mine drainage water, and increased sediment loads discharged to streams. When coal surfaces are exposed,
pyrite comes in contact with water and air and forms
sulfuric acid. As water drains from the mine, the acid moves into the waterways; as long as rain falls on the mine
tailings the sulfuric-acid production continues, whether the mine is still operating or not. Also waste piles and coal storage piles can yield sediment to streams. Surface waters may be rendered unfit for agriculture, human consumption, bathing, or other household uses. There are five principal technologies used to control water flow at mine sites: diversion systems,
ash ponds (surface impoundments), groundwater pumping systems, subsurface drainage systems, and subsurface barriers. In the United States, due to few federal and state regulations concerning ash ponds, most power plants do not use
geomembranes, leachate collection systems, or other flow controls often found in
municipal solid waste landfills. EPA promulgated more stringent requirements for ash ponds and landfills in its first national regulation in 2015. In response to litigation, EPA published final regulations for ash ponds in 2020, requiring unlined ponds to be retrofitted with liners, or using alternatives to ponds for managing ash wastes. A final regulation for inactive surface impoundments was published in 2024.
Water pollution Coal-fired boilers, using either coal or
lignite rich in
limestone, produces
fly ash containing
calcium oxide (CaO). CaO readily dissolves in water to form
slaked lime (Ca(OH)2) which is carried by rainwater to rivers/irrigation water from the ash dump areas.
Lime softening process precipitates Ca and Mg ions / removes temporary hardness in the water and also converts
sodium bicarbonates in river water into sodium carbonate.
Sodium carbonate (washing soda) further reacts with the remaining Ca and Mg in the water to remove / precipitate the total
hardness. Also, water-soluble sodium salts present in the ash enhance the sodium content in water further. Thus river water is converted into
soft water by eliminating Ca and Mg ions and enhancing Na ions by coal-fired boilers. Soft water application in
irrigation (surface or ground water) converts the fertile soils into
alkaline sodic soils. River water alkalinity and
sodicity due to the accumulation of salts in the remaining water after meeting various transpiration and evaporation losses, become acute when many coal-fired boilers and power stations are installed in a river basin. River water sodicity affects downstream cultivated river basins located in China, India, Egypt, Pakistan, west Asia, Australia, western US, etc. Pollutant discharges from ash ponds to surface waters typically include
arsenic,
lead,
mercury,
selenium,
chromium, and
cadmium. In the US, discharges to surface waters from mine drainage, coal storage facilities, coal preparation plants and ash ponds are regulated by permits in the
National Pollutant Discharge Elimination System (NPDES).
Waste management site (aerial photograph of taken the day after the event, 23 December 2008)|alt=Aerial photo of pollution caused by leaking sludge storage pond The burning of coal leaves substantial quantities of fly ash, which is usually stored in ash ponds (wet storage) or landfills (dry storage). Pollutants such as
heavy metals leach into groundwater from unlined ponds or landfills, and can pollute aquifers for decades or centuries. The EPA classified 44 sites in the US as potential hazards to communities. Such a classification means that the waste sites could cause death and significant property damage if an event such as a storm, a terrorist attack or a structural failure caused a spill. EPA estimated that about 300 dry landfills and wet storage ponds are used around the country to store ash from coal-fired power plants. The storage facilities hold the
noncombustible ingredients of coal, including the ash captured by equipment designed to reduce air pollution. In the low-coal-content areas waste forms
spoil tips or slag heaps. The problem of
landslides in spoil tips was first brought to public attention in October 1966 in the
English-speaking world when a slag heap at
Aberfan in
Glamorgan,
Wales, gave way, killing 144 people, 116 of them children. The tip was built over a
spring, increasing its instability, and its height exceeded guidelines. Water from heavy rainfall had built up inside the tip, weakening the structure, until it suddenly collapsed onto a school below. The wider issue of stability had been known about prior to the Aberfan disaster; for example, it was discussed in a paper by Professor
George Knox in 1927, but received little serious consideration by professional engineers and geologists — even to those directly concerned with mining. Also the Aberfan disaster was not the first landslide with casualties: for example, in 1955 two successive landslides killed 73 people in
Sasebo, Nagasaki in Japan.
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Wildlife Surface mining of coal causes direct and indirect damage to wildlife. The impact on wildlife stems primarily from disturbing, removing and redistributing the land surface. Some impacts are short-term and confined to the mine site however others have far-reaching, long-term effects. The most direct effect on wildlife is destruction or displacement of species in areas of excavation and spoil piling. Pit and spoil areas are not capable of providing food and cover for most species of wildlife. Mobile wildlife species like game animals, birds, and predators leave these areas. More sedentary animals like invertebrates, reptiles, burrowing rodents, and small mammals may be destroyed. The community of microorganisms and nutrient-cycling processes are upset by movement, storage, and redistribution of soil. Degradation of aquatic habitats is a major impact by surface mining and may be apparent many miles from a mining site. Sediment contamination of surface water is common with surface mining. Sediment yields may increase a thousand times their former level as a result of strip mining. The effects of sediment on aquatic wildlife vary with the species and the amount of contamination. High sediment levels can kill fish directly, bury spawning beds, reduce light transmission, alter temperature gradients, fill in pools, spread streamflows over wider, shallower areas, and reduce the production of aquatic organisms used as food by other species. These changes destroy the habitat of valued species and may enhance habitat for less-desirable species. Existing conditions are already marginal for some freshwater fish in the United States, and the sedimentation of their habitat may result in their extinction. The heaviest sediment pollution of drainage normally comes within 5 to 25 years after mining. In some areas, unvegetated spoil piles continue to erode even 50 to 65 years after mining. The presence of acid-forming materials exposed as a result of surface mining can affect wildlife by eliminating habitat and by causing direct destruction of some species. Lesser concentrations can suppress productivity, growth rate and reproduction of many aquatic species. Acids, dilute concentrations of heavy metals, and high alkalinity can cause severe damage to wildlife in some areas. The duration of acidic-waste pollution can be long; estimates of the time required to leach exposed acidic materials in the Eastern United States range from 800 to 3,000 years. == Air pollution ==