The Reason and Response for Acid Rain

Acid rain is acid rain. Acid deposition is an increase in acidic amalgam on the earth's surface. It is also basically composed of acid rainwater from sulfur dioxide (SO 2) and other pollutants. Acid rain is formed by releasing sulfur dioxide (SO 2) and nitrogen oxide (NO 2) into the atmosphere. The chemicals are then absorbed by the rain and produce acid rain. Acid rain mainly occurs from chemical substances released into the atmosphere from coal-fired power plants.

When these gases react with water molecules and other chemical substances in the atmosphere, mild acidic compounds such as sulfuric acid and nitric acid are formed and acid rain occurs. Acid rain often causes weathering of buildings, corrosion of metals, and delamination of surface coatings. The eruptive volcano contains chemical substances that may cause acid rain. In addition, human activities, combustion plants and combustion of fossil fuels by cars are another reason behind this activity.

Acid rain generally affects the chemical properties of soil, plant activity and surface water's acidity. In this sense, this means acid rain has a big impact on the environment. Increasing acid rain continues to affect the health of humans and plants, the chemical composition of the soil, and most importantly the survival of aquatic life. The higher the acid concentration, the more severe the result will be. Consistent high levels of acid rain can significantly reduce the life activity of plants and the continuity of aquatic life. The majority of the impact depends on the presence of acidic deposits in the atmosphere and the acidity of various forms of precipitation.

Acid rain has a serious effect on soil chemistry and biology. It is often destroyed or changed due to the influence of soil chemical constituents such as acid rain, soil microorganism, biological activity, soil pH and so on. Soil must maintain optimum pH to allow biological activity to prosper. Therefore, every time acid rain penetrates the soil, the optimum pH changes, thereby reversing chemical and biological activity. Therefore, sensitive soil microorganisms that can not adapt to pH change are killed and soil microbial enzymes are denatured. Higher acidity also elutes important minerals and nutrients such as calcium and magnesium. As a result, the soil loses its quality and composition, making it impossible to support plant life and soil microorganisms.