Moist Air - Density vs. Water Content and Temperature
Density of the mix of dry air and water vapor - moist humid air.
The density of humid air varies with water content and temperature. When the temperature increases a higher molecular motion results in expansion of volume and a decrease of density.
The density of a gas, dry air, water vapor - or a mixture of dry air and water vapor like moist or humid air - can be calculated with the Ideal Gas Law .
Density of Dry Air
The density of dry air can be calculated
ρ a = p a / R a T
= 0.0035 p a / T (1)
where
ρ a = density dry air (kg/m3 )
p a = partial pressure of dry air (Pa, N/m2)
R a = 286.9 - individual gas constant of dry air (J/kg K)
T = absolute dry bulb temperature (K)
Density of Water Vapor
The density of the water vapor can be calculated
ρ w = p w / R w T
= 0.0022 p w / T (2)
where
p w = partial pressure of water vapor (Pa, N/m2)
ρ w = density of water vapor (kg/m3 )
R w = 461.5 - individual gas constant water vapor (J/kg K)
T = absolute dry bulb temperature (K)
Density of Moist Air - an Air Vapor Mixture
The amount of water vapor in air influences the density. Water vapor is relatively light compared to diatomic Oxygen and diatomic Nitrogen - the dominant components in air .
When vapor content increases in moist air the amount of Oxygen and Nitrogen are decreased per unit volume and the density of the mix decreases since the mass is decreasing.
Based on specific volume of moist air the moist air density can be calculated
ρ = 1 / v
= (p / R a T) (1 + x) / (1 + x R w / R a ) (3)
where
v = specific volume of moist air per mass unit of dry air and water vapor (m3 /kg)
x = m w / m a = specific humidity or humidity ratio (kg h2o /kg dry_air )
m w = mass of water vapor (kg)
m a = mass of dry air (kg)
p = pressure in the moist air (Pa)
The density of dry air with the same total pressure p as in the mixture (dry air + vapor partial pressure) - can be calculated as a reference as
ρ ref = p / R a T (4)
where
ρ ref = reference density of dry air with the same pressure as in the air vapor mixture (kg/m3 )
The density of moist air related to dry air can be expressed by combining (4) and (3) as
ρ = ρ ref (1 + x) / (1 + x R w / R a ) (5)
The gas constant ratio between water vapor and air is
R w / R a = (461.5 J/kg K) / (286.9 J/kg K)
= 1.609
and inserting the ratio in (5) the density of moist air related to dry air can be expressed as
ρ = ρ ref (1 + x) / (1 + 1.609 x ) (6)
Note! As we can see from (6) - increased moisture content reduces the density of moist air - dry air is more dense than moist air.
Related Topics
-
Air Psychrometrics
Moist and humid air calculations. Psychrometric charts and Mollier diagrams. Air-condition systems temperatures, absolute and relative humidities and moisture content in air. -
Densities
Densities of solids, liquids and gases. Definitions and convertion calculators. -
Gases and Compressed Air
Properties of air, LNG, LPG and other common gases. Pipeline capacities and sizing of relief valves.
Related Documents
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Air - Humidifying by Adding Steam or Water
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Air - Humidifying with Steam - Imperial Units
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Air - Humidity Measurement from Dry and Wet Bulb Temperature
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Mixing of Humid Air
The change in state wwhen mixing moist air - enthalpy, heat, temperature and specific humidity. -
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Humidity ratio of moist air to humidity ratio of saturated moist air. -
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Density of moist air vs. pressure ranging 75 - 1000 mmHg. -
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The pressure in a mixture of dry air and water vapor - humid or moist air - can be estimated by using Daltons Law of partial pressures. -
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Moist Air - Specific Volume
Specific volume of moist air is defined as the total volume of humid air per mass unit of dry air -
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Specific humidity of moist air vs. relative humidity, water vapor and air density. -
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Saturation pressure of water vapor in moist air vs. temperature. -
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Weight of water vapor in air -
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Wet Steam - Specific Volume
Wet steam and specific volume.