Air gas
Air Gas is a mixture of gases naturally present in the Earth's atmosphere. It primarily consists of nitrogen (78.09%) and oxygen (20.95%), with small amounts of argon (0.93%), carbon dioxide (0.04%), and other trace gases. The composition of air gas can vary depending on the geographical location, altitude, and weather conditions.
Composition[edit | edit source]
The primary components of air gas are nitrogen and oxygen, which together make up approximately 99% of the gas. Nitrogen is a colorless, odorless, tasteless gas that is relatively inert and non-reactive. Oxygen, on the other hand, is a highly reactive gas that is essential for most forms of life on Earth.
In addition to nitrogen and oxygen, air gas also contains trace amounts of other gases. These include argon, carbon dioxide, neon, helium, and methane. The exact composition can vary depending on a variety of factors, including human activity.
Properties[edit | edit source]
Air gas has several important properties that make it vital for life on Earth. It acts as a natural insulator, helping to regulate the planet's temperature. It also provides the oxygen necessary for respiration and combustion, and the carbon dioxide necessary for photosynthesis.
The density of air gas decreases with altitude, which has significant implications for aviation and meteorology. The refractive index of air gas is also important in optics and atmospheric science.
Uses[edit | edit source]
Air gas has a wide range of uses in various industries. It is used in the production of steel, in the operation of internal combustion engines, and in the synthesis of ammonia for fertilizers. It is also used in medical applications, for example in oxygen therapy and anesthesia.
In addition, air gas is used in a variety of scientific research applications. These include atmospheric science, climate research, and the study of air pollution.
See also[edit | edit source]
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Contributors: Prab R. Tumpati, MD