Air
Air is the invisible mixture of gases that surrounds the Earth and is vital for all living organisms. It is primarily composed of nitrogen (78%), oxygen (21%), and small amounts of other gases such as argon, carbon dioxide, and water vapor.
Composition[edit | edit source]
The composition of air is relatively constant up to an altitude of about 10,000 meters. The primary components are:
- Nitrogen (N2) - 78.08%
- Oxygen (O2) - 20.95%
- Argon (Ar) - 0.93%
- Carbon dioxide (CO2) - 0.04%
- Trace amounts of other gases including neon, helium, methane, krypton, and hydrogen.
Properties[edit | edit source]
Air has several important properties:
- It is a fluid and can flow from one place to another.
- It has mass and weight.
- It exerts pressure, known as atmospheric pressure.
- It can be compressed and expanded.
- It is essential for combustion and respiration.
Atmospheric Layers[edit | edit source]
Air is divided into several layers based on temperature and composition:
- Troposphere: The lowest layer where weather occurs and where most of the air mass is found.
- Stratosphere: Contains the ozone layer which absorbs and scatters ultraviolet solar radiation.
- Mesosphere: The layer where most meteors burn up upon entering the Earth's atmosphere.
- Thermosphere: A layer with very thin air, where the auroras occur.
- Exosphere: The outermost layer, where air molecules are sparse and can escape into space.
Importance[edit | edit source]
Air is crucial for:
- Respiration: All aerobic organisms require oxygen to produce energy.
- Photosynthesis: Plants use carbon dioxide and release oxygen.
- Climate: Air circulation patterns influence weather and climate.
- Sound: Air is the medium through which sound waves travel.
Air Pollution[edit | edit source]
Air pollution is the presence of harmful substances in the air, which can have adverse effects on health and the environment. Common pollutants include:
See Also[edit | edit source]
References[edit | edit source]
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Contributors: Prab R. Tumpati, MD