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Humidity - or moist - is the water vapor present in air. Commonly used terms are Absolute, Specific and Relative Humidity
The density and the specific volume of air varies with the elevation above sea level
Specific Heat of air at constant temperature 20oC and pressure ranging 0.01 to 100 atm
Dry air is a mechanical mixture of nitrogen, oxygen, carbon dioxide and more
Amount of vapor (lb/h in 100 cfm) in humid air
Temperature, density, specific heat, thermal conductivity, expansion coefficient, kinematic viscosity and Prandtl's number for temperatures ranging -150 - 400 oC
An introduction to air psychrometrics
Basic air condition processes - heating, cooling, mixing, humidifying and dehumidifying by adding steam or water - psychometric diagrams and the Mollier charts
Transforming between psycrometric charts and Mollier diagrams
The maximum cooling tower efficiency is limited by the wet-bulb temperature of the cooling air
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Cooling and dehumidifying processes of moist and humid air - sensible and latent cooling
Pressure in a mixture of dry air and water vapor - humid or moist air - can be estimated by using Daltons Law of Partial Pressures
A dehumidification tutorial with psychrometric charts
Classification of dehumidifiers
Densities and specific volumes of dry air and water vapor at temperatures ranging 225 to 900 degF (107 to 482 degC)
Calculate the density of dry air, water vapor or the mixture of air and water vapor - moist or humid air
Density of moist air - pressure ranging 75 - 1000 mm Hg
Dry Bulb, Wet Bulb and Dew Point temperatures are commonly used to determine the state of humid moist air
The Drying Force 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 - enthalpy is used to calculate cooling and heating processes
The amount of evaporated water from a water surfaces - like swimming pools or an open tanks - depends on the temperature in the water and in the air, and the humidity and velocity of the air above the surface - online calculator
An evaporative cooling tutorial
The Great Sensible Heat Factor is the ratio between the sensible and total heat for a cooling coil
Moisture - temperature and heat humidity factor
Heat removed with air - dry and wet bulb temperature
Calculating enthalpy change and temperature rise when heating moist and humid air without adding moisture
The Ideal Gas Law relating pressure, temperature, and volume of an ideal or perfect gas used for air with water vapor - or moist air
Air can be humidified by adding water or steam
The amount of vapor - kg per cubic meter - in humid air
Humidity ratio (GPP) is the ratio between actual mass of water vapor present in moist air - to the mass of dry air
In perfect or ideal gas the change in density is directly related to the change of temperature and pressure as expressed by the Ideal Gas Law
Latent heat is the heat, when supplied to or removed from air, results in a change of moisture content - the temperature of the air is not changed
Moisture limit in air varies with temperature
Measuring relative air humidity with dry and wet bulb temperatures
Calculating enthalpy, heat, temperature and specific humidity in mixing humid air
A psychrometric table with moist humid air properties
The ratio of humidity ratio of moist air to humidity ratio of saturated moist air - the Degree of Saturation
Mole fraction of water vapor expresses 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
The Mollier diagram is a graphic representation of the relationship between air temperature, moisture content and enthalpy - and is a basic design tool for building engineers and designers
Outdoor design temperature and relative humidity in US states and cities - summer and winter
The relationship between outdoor and indoor temperature rise - and the effect on the relative humidity
Heat Gain from Occupants in Air Conditioned Spaces - in btu/hr
Metabolic heat gain from occupants in air conditioned spaces at different degrees of activities - in Watts
Air pressure and maximum content of water in saturated air
A psychrometric chart in English units - temperature ranging from 20oF to 120oF
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
Dry and wet bulb temperature, pressure and weight saturated water vapor and air saturated with water vapor
Dry Bulb and Wet Bulb Temperature, Specific Volume, Relative Humidity, Enthalpy and more ..
Recommended indoor effective temperatures at various outdoor dry-bulb temperatures
Recommended indoor effective temperatures at various outdoor dry-bulb temperatures
Recommended Relative Humidity - RH - in production and process environments like libraries, breweries, storages and more
The relative humidity of air 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
Specific heat 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
Calculating specific humidity of moist air knowing relative humidity, water vapor and air density
Vapor pressures in moist air from dry and wet bulb temperatures
Pressure loss due to friction
Water saturation pressure at temperatures ranging 0 - 100 oC and 32 - 700 oF - Imperial and SI Units
Weight of water vapor in air
The saturation pressure of water vapor in moist air varies with temperature
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