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At 101.325 kPa (abs) and 15 °C (59 °F), air has a density of approximately 1.225 kg/m 3 (0.0765 lb/cu ft), which is about 1 ⁄ 800 that of water, according to the International Standard Atmosphere (ISA).
Online calculator, figures and tables showing density, specific weight and thermal expansion coefficients of air at temperatures ranging -100 to 1600 °C (-140 to 2900 °F) at atmospheric and higher pressure - Imperial and SI Units.
Online calculator, figures and tables showing density, specific weight and thermal expansion coefficients of air at temperatures ranging -100 to 1600 °C (-140 to 2900 °F) at atmospheric and higher pressure - Imperial and SI Units.
International Standard Atmosphere properties like pressure, temperature, density, viscosity, thermal conductivity and velocity of sound are indicated below. ρo = 1.2250 kg/m3.
Pure, dry air has a density of 1.293 kg m−3 at a temperature of 273 K and a pressure of 101.325 kPa. Apart from the variability of water vapor, the composition of air is essentially constant to an altitude of at least 50 km.
The ISA or International Standard Atmosphere states the density of air is 1.225 kg/m3 at sea level and 15 degrees C. The IUPAC uses an air density of 1.2754 kg/m3 at 0 degrees C and 100 kPa for dry air.
Use the online air density calculator to find out the density of air at any given temperature and pressure.
Pressure, temperature, density, viscosity and speed of sound variation for the international standard atmosphere (ISA) can be calculated for a range of altitudes from sea level upward. This is done using an exact solution to the hydrostatic equation for a column of air.
Typical values of the density, pressure, and temperature of air at sea level static conditions for a standard day are: Density: 1.229 kilogram per cubic meter or .00237 slug per cubic feet. Specific Volume: .814 cubic meters per kilogram or 422 cubic feet per slug. Pressure: 101.3 kilo Newtons per square meter or 14.7 pounds per square inch
Air Density and Specific Weight Table, Equations and Calculator: The density of air, ρ (Greek: rho) (air density), is the mass per unit volume of Earth's atmosphere. Air density, like air pressure, decreases with increasing altitude. It also changes with variation in temperature or humidity.