
Nature can indeed cause pollution. While pollution is often associated with human activity, natural events such as forest fires and active volcanoes can also cause environmental pollution. However, the word pollution typically implies contaminants with an anthropogenic source, and human activities are the predominant cause of pollution today. Air pollution, water pollution, and land pollution are the three primary forms of environmental pollution, and they can have detrimental effects on human health, wildlife, and the environment.
Characteristics | Values |
---|---|
Nature can cause pollution through | Smoke from wildfires, ash and gases from volcanic eruptions, gases like methane emitted from decomposing organic matter in soils |
Human-made air pollution sources | Vehicle emissions, fuel oils and natural gas, manufacturing by-products, power generation, chemical production, coal-fueled power plants, industrial boilers, refineries |
Air pollution effects | Oxidative stress, inflammation in human cells, respiratory issues, asthma, cardiac problems, emergency department visits, hospital admissions, lung damage, cancer, neurological disorders, immune system disorders, osteoporosis, reproductive issues, developmental issues |
Progress in reducing air pollution | The US has made progress in reducing air and water pollution since the 1960s, with success in controlling point-source pollutants; the EU has also made significant progress in recent decades |
What You'll Learn
Volcanic eruptions release ash and gases
The physical characteristics of volcanic ash make it a highly disruptive pollutant. Ash is hard, abrasive, mildly corrosive, and electrically conductive when wet. Its fine particles can cause respiratory issues, eye and skin irritation, and other negative health effects, particularly for those with pre-existing conditions. Ingesting ash can be harmful to livestock, causing dental issues and, in cases of high fluorine content, fluorine poisoning.
Volcanic eruptions also release gases, including water vapour, carbon dioxide, and sulfur dioxide, among others. These gases can rise tens of kilometres into the Earth's atmosphere and spread even further through wind. The most hazardous gases to people, animals, and the environment are sulfur dioxide, carbon dioxide, and hydrogen fluoride. Sulfur dioxide can cause skin and eye irritation and respiratory issues, while carbon dioxide, being heavier than air, can collect in low-lying areas, posing lethal risks to people, animals, and vegetation. Hydrogen fluoride, a powerful irritant, can cause conjunctivitis, skin irritation, bone degeneration, and tooth damage.
The release of volcanic ash and gases during eruptions has significant impacts on critical infrastructure and various sectors of society. Ash can disrupt power supply systems, transportation, water treatment and supply, and telecommunication networks. It can also affect agriculture, inhibiting plant growth and contaminating water sources. The weight of ash accumulation can cause structural damage to buildings and collapse roofs. Additionally, volcanic gases contribute to air pollution and acid rain, further exacerbating the environmental and health impacts.
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Wildfires produce smoke and fumes
The particles in wildfire smoke can be grouped into two main categories: coarse particles and fine particles. Coarse particles are generally larger than 2.5 micrometres and smaller than or equal to 10 micrometres in diameter. While coarse particles are primarily generated from mechanical operations such as construction and agriculture, a small percentage is present in wildfire smoke. Fine particles, on the other hand, are generally 2.5 micrometres or smaller in diameter and represent the main pollutant emitted from wildfire smoke, comprising approximately 90% of the total particle mass. These fine particles are of the greatest health concern as they can travel deep into the respiratory tract, reaching the lungs.
The health effects of inhaling wildfire smoke can be immediate and serious. In the short term, smoke can irritate the eyes, nose, and throat, and cause nausea. Studies have also shown that exposure to heavy smoke can lead to temporary changes in lung function, making breathing more difficult. Additionally, inhaling carbon monoxide, a common substance in smoke, decreases the body's oxygen supply and can cause headaches, reduced alertness, and aggravate heart conditions. Fine particles from smoke can also cause respiratory irritation and shortness of breath, as well as worsen existing medical conditions such as asthma and heart disease. Physical exertion during exposure to smoke can further exacerbate these health effects.
The long-term health effects of exposure to wildfire smoke are also a concern. People who live in areas with higher fine particulate air pollution and those who breathe air containing fine particles over long periods have an increased risk of cardiovascular disease and mortality. Frequent exposure to smoke, even for brief periods, has been linked to a higher risk of cancer, lung disease, and cardiovascular disease in some studies. Therefore, it is crucial for individuals to take precautions to limit their exposure to wildfire smoke and to seek medical attention if they experience any adverse health symptoms.
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Decomposing organic matter emits methane
In natural environments, such as wetlands, flooded soils, and the digestive tracts of ruminant animals, methane production by bacteria is a common occurrence. However, human activities can also contribute to this process. For example, in landfills, large amounts of organic waste are buried and compacted, creating an anaerobic environment that leads to methane emissions. This is particularly concerning as methane has a much higher global warming potential than carbon dioxide, the primary greenhouse gas emitted by aerobic decomposition.
To mitigate methane emissions from decomposing organic matter, providing adequate oxygen is essential. In compost piles, for instance, actively turning or aerating the compost encourages the production of carbon dioxide instead of methane. Additionally, the use of specific composting methods, such as open pile, static pile, in-vessel, windrow, and vermicomposting, can help minimize methane production.
While it is impossible to eliminate methane emissions entirely from decomposing organic matter, proper management practices can significantly reduce their impact on the environment. By understanding the role of oxygen in decomposition and employing suitable techniques, we can minimize methane emissions and promote more sustainable practices.
Furthermore, the methane produced during anaerobic decomposition can be captured and utilized for energy generation. Through processes like gas collection from manure swamps, wastewater treatment, and landfills, methane can be collected, filtered, and burned to produce electricity. This not only reduces the amount of methane released into the atmosphere but also provides a valuable energy source.
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Coal-burning power plants release mercury
Nature can indeed cause pollution. For example, volcanoes and forest fires release mercury into the atmosphere. However, human activities are responsible for much of the mercury that is released into the environment. The burning of coal, oil, and wood as fuel, as well as the burning of mercury-containing waste, can cause mercury to become airborne.
Coal-burning power plants are a significant source of mercury emissions, particularly in the United States. When coal is burned to generate electricity, the mercury it contains becomes airborne and enters the atmosphere. According to the 2014 National Emissions Inventory, power plants that burn coal account for about 44% of all anthropogenic mercury emissions in the US.
Mercury is a naturally occurring chemical element found in rock in the Earth's crust, including coal deposits. When coal is burned, the mercury is released and becomes a problem for the environment when it enters the atmosphere and water. Mercury can also be released into the air through the burning of oil, wood, and waste that contains mercury.
The amount of mercury deposited in a given area depends on the amount released from local, regional, national, and international sources. Mercury in the atmosphere can be transported over various distances, from a few feet to halfway around the globe, before it is deposited in soil or water. This long-range transport is known as the "global cycle."
Mercury emissions from coal-burning power plants have significant ecological and health impacts. Birds and mammals that eat fish, such as eagles, otters, and endangered Florida panthers, are at risk of exposure to high levels of methylmercury, a highly toxic form of mercury. High levels of methylmercury can cause reduced reproduction and slower growth and development in these animals.
Human exposure to mercury primarily occurs through the consumption of fish and shellfish with high levels of methylmercury. Breathing mercury vapour is another, less common way that people are exposed. High levels of mercury exposure can harm the brain, heart, kidneys, lungs, and immune system of people of all ages. In babies and young children, high levels of methylmercury in the bloodstream may affect their developing nervous systems, impacting their ability to think and learn.
To reduce mercury emissions from coal-burning power plants, regulations and a decrease in mercury use have been implemented. For example, the burning of municipal and medical waste, which was once a major source of mercury emissions, has been reduced by over 95% due to a reduction in mercury use and state and federal regulations.
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Natural processes cause climate change
Natural processes and phenomena have influenced climate change throughout Earth's history. Over the course of Earth's existence, volcanic eruptions, fluctuations in solar radiation, tectonic shifts, and even small changes in the planet's orbit have all contributed to observable effects on planetary warming and cooling patterns.
Volcanic Eruptions
Volcanoes play a significant role in climate change through the emission of gases and particles during eruptions. The impact of volcanic activity on the climate depends on how sunlight interacts with the released volcanic material. Large explosive eruptions can inject particles such as sulphur dioxide (SO2) into the upper atmosphere, where they reflect sunlight back into space, leading to a cooling effect on the planet for several years. On the other hand, volcanic gases like carbon dioxide (CO2) have the potential to cause global warming. However, in the present day, volcanic emissions of CO2 contribute very little to atmospheric CO2 levels, accounting for about 1% of anthropogenic emissions.
Solar Radiation and Orbital Variations
Variations in solar activity and changes in the Earth's orbit and axial tilt (collectively known as Milankovitch cycles) influence the amount of solar heat that reaches the Earth's surface, subsequently affecting climatic patterns. The sun's energy output is not constant and undergoes natural 11-year cycles of small ups and downs in intensity. While these variations can impact the Earth's climate, they have played a minor role in the climate changes observed in recent decades. Additionally, changes in the Earth's orbit, such as eccentricity (deviation from a circular orbit), axial tilt (obliquity), and precession (wobble caused by the gravitational pull of the Moon and the Sun), occur over much longer periods and have more substantial effects on climatic variations, including ice ages.
Tectonic Shifts and Mountain Formation
Over long periods, plate tectonic processes cause the movement of continents, leading to changes in their positions on the Earth. For example, the British Isles were near the equator during the Carboniferous Period, resulting in a warmer climate than today. Tectonic activity also contributes to the formation of mountains, which can influence the circulation of air around the globe and consequently impact regional climates.
While these natural processes have influenced climate change throughout Earth's history, it is important to note that recent climate changes, especially since the Industrial Revolution, cannot be explained by natural causes alone. Human activities, such as the burning of fossil fuels and deforestation, have become the dominant drivers of the observed warming trends over the past century.
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