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Liquid air

Air that has been condensed into a liquid

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Through Atmosphere of Earth, Vacuum flask and Nitrogen

Properties

Liquid air has a density of approximately 870 kg/m3 (870 g/L; 0.87 g/cm3). The density of a given air sample varies depending on the composition of that sample (e.g., humidity & CO2 concentration). Since dry gaseous air contains approximately 78% nitrogen, 21% oxygen, and 1% argon, the density of liquid air at standard composition is calculated by the percentage of the components and their respective liquid densities (see liquid nitrogen and liquid oxygen). Although air contains trace amounts of carbon dioxide (about 0.0425%), carbon dioxide solidifies from the gas phase without passing through the intermediate liquid phase, and hence will not be present in liquid air at pressures less than 5.1 atm (520 kPa).

The boiling point of air is 78.80 K (−194.35 °C; −317.83 °F), intermediate between the boiling points of liquid nitrogen and liquid oxygen. However, it can be difficult to maintain a stable temperature as the liquid boils, since nitrogen will boil off first, leaving the mixture oxygen-rich and altering the boiling point. This may also occur in some circumstances due to liquid air condensing oxygen from the atmosphere.

Liquid air starts to freeze at approximately 60 K (−213.2 °C; −351.7 °F), precipitating nitrogen-rich solid (but with an appreciable amount of oxygen in solid solution). Unless the oxygen is previously accommodated in the solid solution, the eutectic freezes at 50 K (−223.2 °C; −369.7 °F).

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