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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.
This is a look at the density of air at STP, the factors that affect air density, and how it is changed by temperature, pressure, and water vapor.
Density and specific volume of air varies with elevation above sea level. Relative humidity in moist air can estimated by measuring the dry and wet bulb temperature. Figures and tables with isobaric (Cp) and isochoric (Cv) specific heat of air at constant temperature and pressure ranging 0.01 to 10000 bara.
Use the online air density calculator to find out the density of air at any given temperature and pressure.
At 101.325 kPa (abs) and 20 °C (68 °F), air has a density of approximately 1.204 kg/m 3 (0.0752 lb/cu ft), according to the International Standard Atmosphere (ISA).
Q.1. What is the air density at standard temperature and pressure? Ans. The air density at STP is 1.2754 kg/m 3.
At sea level and at 15 °C, air has a density of approximately 1.225 kg/m 3 (0.001225 g/cm 3, 0.0023769 slug/ft 3, 0.0765 lbm/ft 3) according to ISA (International Standard Atmosphere). Specific weight and density of air at standard atmospheric pressure - Imperial 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.
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.
Standard air density is density of air calculated at standard temperature and pressure conditions. Standard temperature and pressure (STP) conditions are used as reference points in thermodynamics of gases.