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Humidity or moist is the water vapor present in air. Common used terms are the Absolute, Specific and Relative Humidity.
The density and the specific volume of air varies with the elevation above sea level
Dry air is a mechanical mixture of nitrogen, oxygen, carbon dioxide and more
The amount of vapor (lb/h in 100 cfm) in humid air
Air properties - temperature, density, specific heat, thermal conductivity, expansion coefficient, kinematic viscosity and Prandtl number for temperatures between -150oC and 400oC.
An introduction to air psychrometrics
Overview of the basic changes of air conditions by heating, cooling, mixing, humidifying and dehumidifying air by adding steam or water. The different processes are shown in psychometric diagram and the Mollier chart.
Common psychometric terms as Dry Bulb and Wet Bulb Temperature, Specific Volume, Relative Humidity and Enthalpy
How to transform between the psycrometric chart and the Mollier chart.
The cooling and dehumidifying process of moist and humid air. Sensible and Latent Cooling
The maximum cooling tower efficiency depends on the wet-bulb temperature of the air
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A dehumidification tutorial with psychrometric charts
Classification of dehumidifiers
Calculating the density of dry air, water vapor or the mixture of air and water vapor - moist or humid air
Dry Bulb, Wet Bulb and Dew Point temperatures are commonly used to determine the state of humid moist air.
The Drying Force (or Effect) of air may be expressed as the moisture holding capacity of the air and the evaporation capacity from a water surface to the air
The enthalpy of moist and humid air consist of sensible heat and latent heat. The enthalpy is important for calculating cooling and heating processes
The amount of evaporated water from a water surface - as a swimming pool or an open tank - depends on the temperature in the water and in the air, and the humidity and velocity of the air above the surface
An evaporative cooling tutorial
The Great Sensible Heat Factor is the ratio between the sensible and total heat for a cooling coil
Calculating enthalpy change and temperature rise when sensible heating moist and humid air
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The Ideal Gas Law relating pressure, temperature, and volume of an ideal or perfect gas can also be used for air with water vapor - moist air
Air can be humidified by adding water or steam
The amount of vapor - kg per cubic meter - in humid air
Humidity ratio is the ratio between actual mass of water vapor present in moist air - to the mass of dry air
Latent heat is the heat that when supplied to, or removed from air, there is a change in the moisture content of the air, but the temperature of the air is not changed
How to measure relative air humidity with dry and wet bulb temperatures
Calculating enthalpy, heat, temperature and specific humidity when mixing humid air
The ratio of the humidity ratio of moist air to the humidity ratio of saturated moist air - is called the Degree of Saturation
Psychrometric Table of Moist Humid Air Properties
The mole fraction of water vapor express the ratio of water molecules to air and water molecules.
Dry air is a mixture of gases where the molecular weight can be calculated by adding the weight of each component
An online psychrometric calculator in SI and English Units
The relationship outside and inside temperature - and relative humidity
Approximate Heat Gain from Occupants in Air Conditioned Spaces - in btu/hr
Approximate metabolic heat gain from occupants in air conditioned spaces at different degrees of activities - in watts
The pressure in a mixture of dry air and water vapor - humid or moist air - can be estimated by using Daltons Law
A psychrometric chart in English units - temperature ranging from 20oF to 120oF
A word document with a psychrometric chart that can be resized.
The psychrometric chart or the Mollier diagram graphically represents the interrelation of air temperature and moisture content and is a basic design tool for building engineers and designers
Psychrometric Chart in I-P Units at high temperature at sea level and barometric pressure 29.921 Inches of HG
Psychrometric chart in I-P Units at low temperature at sea level and barometric pressure 29.921 Inches of HG
Psychrometric chart in I-P Units at 5000 feet and barometric pressure 24.896 Inches of HG
Psychrometric chart in I-P Units at 7500 feet and barometric pressure 22.653 Inches of HG
Sea Level Psychrometric Chart - Ledger Size - Both US and SI units
A downloadable psychrometric chart at normal temperatures in SI Units
An psychrometric chart with extended range.
Air conditions can be characterized by using the psychrometric chart. Properties on the chart include dry-bulb and wet-bulb temperatures, relative humidity, humidity ratio, specific volume, dewpoint temperature and enthalpy
Calculate moist air properties in both SI and Imperial units with this online calculator
Recommended indoor effective temperatures for various outside dry-bulb temperatures
Recommended Relative Humidity - RH - limits in production and process environments like libraries, breweries, storages and more
Relative humidity can be expressed by partial vapor and air pressure, density of the vapor and air, or by the actual mass of the vapor and air
The Room Sensible Heat Factor - RSHF - is defined as the sensible heat load in the room divided by the total heat load in room
Sensible heat is dry heat causing change in temperature but not in the moisture content
Sensible Heat Ratio - SHR - is defined as the sensible heat or cooling load divided by the total heat or cooling load
The Specific Heat Capacity of dry air varies with temperature.
Specific volume is defined as the total volume of humid air per mass unit of dry air.
The moisture holding capacity of air varies with temperature
Calculate the specific humidity of moist air knowing the relative humidity, water vapor and air density
Outdoor temperatures and relative humidity's in different US states and cities summer and winter
Water saturation pressure at temperatures ranging 0 - 100 deg C and 32 - 700 deg F, in Imperial and SI Units
Weight of water vapor in air
The saturation pressure of water vapor in moist air vary with temperature.
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