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Air - Moisture Holding Capacity vs. Temperature

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The moisture holding capacity of air increases dramatically with increased temperature as indicated in the diagrams below.

Air Moisture Holding Capacity - SI Units

Moisture holding capacity of air - kg water per kg dry air:

.

Air Moisture Holding Capacity - Imperial Units

Moisture holding capacity of air - lb water per lb dry air:

Moisture holding capacity of air - lb water per 1000 cubic feet dry air:

Note - the moisture holding capacity of air at 100oF (38 oC) is 10 times the moisture holding capacity of air at 30oF (~ 0 oC). This is a very important observation - especially when working with drying processes where air is used to transport moisture away from process and products.

In general

  • it is in general good energy economy to increase the air temperature in a dryer as much as possible! - the increased moisture transport capacity of air at higher temperature out-weights the increased energy-consumption for heating the dry air to higher temperature!
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Dry air is a mechanical mixture of nitrogen, oxygen, argon and several other gases in minor amounts.

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Air density at pressure ranging 1 to 10 000 bara (14.5 - 145000 psi) and constant selected temperatures.

Air - Density, Specific Weight and Thermal Expansion Coefficient vs. Temperature and Pressure

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.

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Diffusion coefficients (D12) for gases in large excess of air at temperatures ranging 0 - 400 °C.

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The drying force of air depends on the air moisture holding capacity and the water surface to air evaporation capacity.

Air - Dynamic and Kinematic Viscosity

Online calculator, figures and tables with dynamic (absolute) and kinematic viscosity for air at temperatures ranging -100 to 1600°C (-150 to 2900°F) and at pressures ranging 1 to 10 000 bara (14.5 - 145000 psia) - SI and Imperial Units.

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Estimate the amount of steam required (lb/h in 100 cfm) in humid air.

Air - Humidifying with Steam, SI units

Using steam to humidify air.

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The mass of water vapor present in moist air - to the mass of dry air.

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Prandtl number for air vs. temperature and pressure.

Air - Properties at Gas-Liquid Equilibrium Conditions

Properties of air change along the boiling and condensation curves (temperature and pressure between triple point and critical point conditions). An air phase diagram included.

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Online calculator with figures and tables showing air thermal conductivity vs. temperature and pressure. SI and imperial units.

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Figures and tables withdry air thermal diffusivity vs. temperarure and pressure. SI and Imperial units.

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Water may condensate when air is cooled in air conditioning systems.

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Maximum cooling tower efficiency is limited by the cooling air wet-bulb temperature.

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Thermodynamic properties of dry air - specific heat, ratio of specific heats, dynamic viscosity, thermal conductivity, Prandtl number, density and kinematic viscosity at temperatures ranging 175 - 1900 K.

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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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Psychrometric table with humid air properties like saturation pressure, specific volume, enthalpy and entropy.

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Relative humidity in moist air is the ratio of partial vapor pressure to air pressure.

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