
Acid rain is a broad term that includes any form of precipitation with acidic components, such as sulfuric or nitric acid, that falls to the ground from the atmosphere in wet or dry forms. It is caused by the emission of sulfur dioxide (SO2) and nitrogen oxides (NOx) into the atmosphere, which react with water, oxygen, and other chemicals to form sulfuric and nitric acids. These acids fall to the earth as wet and dry deposition, causing harmful effects on soil, forests, streams, and lakes. The pH scale, which measures acidity and basicity, ranges from 0 to 14, with 7 being neutral. Values below 7 indicate acidity, while values above 7 indicate basicity. Ocean acidification, caused by increased levels of carbon dioxide in the atmosphere, is another example of pollution causing acidification. This has far-reaching implications for marine life, especially for organisms that rely on calcium and carbonate ions to build shells and skeletons.
| Characteristics | Values |
|---|---|
| Nature of pollution | Acidic |
| pH range | 0-14 |
| pH value indicating acidity | <7 |
| pH value indicating basicity | >7 |
| pH value indicating neutrality | 7 |
| pH of ocean water | 8.1 |
| pH scale | Inverse of hydrogen ion concentration |
| Acid rain | A form of pollution caused by emissions of SO2 and NOx |
| Effects of acid rain | Harmful to soil, forests, streams, lakes, plants, wildlife, and human health |
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What You'll Learn

Acid rain
The acidic compounds can be spread over long distances by wind, affecting both urban and rural areas. When acid rain reaches the Earth, it flows across the surface, enters water systems, and seeps into the soil, causing various ecological and environmental impacts. Acid rain can harm forests and lakes, making waters more acidic and increasing the absorption of aluminium from the soil, which is toxic to aquatic life. It also strips the soil of essential nutrients, such as calcium and magnesium, necessary for plant growth and healthy soil.
In addition to environmental damage, acid rain can also impact human infrastructure and health. It causes corrosion and weathering of buildings, statues, and other structures made of stone, steel, or limestone. Acid rain can also cause health issues in humans, including eye irritation and asthma, especially when present in inhalable fog.
The adverse effects of acid rain have been recognized since the 1960s, and governments in Europe and North America have implemented regulations to reduce sulfur dioxide and nitrogen oxide emissions. These efforts have shown positive results, with significant reductions in sulfur dioxide emissions over time.
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Acid deposition
Wet deposition, or acid rain, is the most common form of acid deposition and occurs when acidic particles are removed from the atmosphere by precipitation, such as rain, snow, or hail. The formation of sulfuric and nitric acids in the atmosphere can be attributed to the combustion of fossil fuels, such as coal-burning power plants, factories, and automobiles. These acidic compounds can be spread over long distances through the atmosphere by winds, leading to widespread ecological damage.
Dry deposition, on the other hand, occurs when acidic particles and gases deposit from the atmosphere in the absence of moisture. This can happen through direct impaction on surfaces such as water bodies, vegetation, or buildings. The accumulated acids on these surfaces can then be washed off by rainfall, leading to harmful effects on plants, wildlife, and water bodies. Dry deposition is more prevalent in areas with lower rainfall, such as desert regions.
The effects of acid deposition have been recognized since the 1970s, with public awareness in the US increasing after reports by The New York Times. International control measures, such as the UNECE Convention on Long-range Transboundary Air Pollution (CLRTAP) and the EU National Emission Ceilings Directive (NECD), have helped reduce emissions contributing to acid deposition. However, acid deposition remains a concern, and the only way to combat it effectively is by curbing the release of pollutants, reducing the burning of fossil fuels, and implementing air-quality standards.
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Ocean acidification
When CO2 is absorbed by seawater, a series of chemical reactions occur, resulting in an increased concentration of hydrogen ions. This increase in hydrogen ions leads to a decrease in pH, making the seawater more acidic. This process is known as ocean acidification and has been referred to as the "evil twin of global warming" and "the other CO2 problem".
The impact of ocean acidification is particularly detrimental to marine calcifiers, including mollusks, oysters, corals, and other shelled organisms. These organisms rely on calcium carbonate to build their shells and skeletons. As the ocean becomes more acidic, the availability of carbonate ions decreases, making it more challenging for these organisms to build and maintain their structures. If the pH drops too low, shells and skeletons may even begin to dissolve. This endangers coral reefs and broader marine ecosystems, affecting food chains linked to the oceans and the livelihoods of people who depend on fishing and coastal management services.
While some species are harmed by ocean acidification, algae and seagrasses may benefit from higher CO2 conditions as they require CO2 for photosynthesis. Ongoing research is examining whether growing seaweed can help slow down the process of ocean acidification. However, the overall impact of ocean acidification on marine life is concerning, with potential consequences for immune responses, reproduction, and the health of marine ecosystems.
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pH scale
The pH scale is a logarithmic scale used to measure how acidic or basic a substance is. The scale runs from 0 to 14, with 7 considered neutral. A pH of less than 7 indicates acidity, while a pH greater than 7 indicates a base or alkalinity. The lower the pH, the more acidic the substance, and the higher the pH, the more basic it is. Each whole pH value represents a tenfold change in acidity or basicness. For example, a substance with a pH of 5 is ten times more acidic than a substance with a pH of 6.
Pure water has a pH of 7 at 25°C, making it neutral. When an acid is dissolved in water, the pH drops below 7, while adding a base or alkali increases the pH above 7. Strong acids, such as hydrochloric acid, can have a pH of 0, while strong alkalis like sodium hydroxide can reach a pH of 14.
The pH scale measures the relative amount of free hydrogen and hydroxyl ions in a substance. Substances with a higher concentration of free hydrogen ions are more acidic, while those with more free hydroxyl ions are more basic. The scale can be applied to liquids, gases, and even solids, providing a common reference standard for different substances.
The pH of water is particularly important for assessing water quality. Natural waters can have varying pH levels depending on their sources and chemical properties. For example, seawater has unique chemical properties that complicate pH measurements, and multiple pH scales are used in chemical oceanography to account for these differences.
Pollution can significantly impact the pH of the environment, particularly through the formation of acid rain. Acid rain occurs when sulfur dioxide (SO2) and nitrogen oxides (NOx) are released into the atmosphere, often from burning fossil fuels. These pollutants react with water, oxygen, and other chemicals to form sulfuric and nitric acids. The acidic compounds can spread over long distances through the atmosphere and fall back to Earth through wet or dry deposition. Acid rain can harm soil, forests, streams, lakes, and other aquatic environments, as well as physical structures and human health.
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Acidic pollutants
The burning of fossil fuels, such as coal, by power plants, factories, and automobiles, releases these acidic pollutants. Acid rain has been observed to have detrimental effects on the environment, particularly on aquatic ecosystems, forests, and wildlife. It can also damage physical structures, such as buildings and cars, and negatively impact human health when inhaled.
When acid rain falls to Earth, it flows across the surface, entering water systems and seeping into the soil. This process increases the solubility of aluminium in the soil, which is then carried into lakes and streams, making the water toxic to aquatic animals. Acid rain also weakens trees by dissolving nutrients in the soil, making them more vulnerable to pests, diseases, and extreme temperatures.
The effects of acid rain have been recognised since the 17th century, when John Evelyn noted the corrosive impact of polluted air on limestone and marble. The term "acid rain" was coined in 1872 by Robert Angus Smith, who first demonstrated the connection between acid rain and atmospheric pollution in Manchester, England. Since then, acid rain has become a widespread issue due to population and industrial growth, with tall smokestacks contributing to the long-range dispersal of acidic pollutants.
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Frequently asked questions
Acid rain is a broad term for any form of precipitation with acidic components, such as sulfuric or nitric acid, that falls to the ground from the atmosphere in wet or dry forms. This can include rain, snow, fog, hail, or even dust. It is caused by the emission of sulfur dioxide (SO2) and nitrogen oxides (NOx) into the atmosphere, which react with water, oxygen, and other chemicals to form sulfuric and nitric acids.
Acid rain can have various ecological effects, particularly on lakes, streams, wetlands, and other aquatic environments. It makes these waters more acidic, increasing the absorption of aluminum from the soil, which is then carried into lakes and streams, making the waters toxic to aquatic animals. Acid rain also damages vegetation, trees, and plants, leaving them more vulnerable to insects and diseases. It can also harm physical structures such as buildings and cars.
Ocean acidification refers to the increasing acidity of the ocean due to the absorption of carbon dioxide (CO2) from the atmosphere. As human activities such as burning fossil fuels and deforestation increase atmospheric CO2 levels, the ocean absorbs more CO2, leading to a decrease in pH and increased acidity. This process has far-reaching implications for marine organisms, particularly those that rely on calcium and carbonate ions to build shells and skeletons, such as oysters and corals.











































