Formula Used:
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The partial pressure of water vapor is the pressure exerted by water vapor in a mixture of gases. It's a crucial parameter in psychrometrics and HVAC calculations, representing the contribution of water vapor to the total pressure of moist air.
The calculator uses the formula:
Where:
Explanation: This formula calculates the partial pressure of water vapor based on the relationship between dry bulb temperature, wet bulb temperature, and the saturation pressure at wet bulb temperature.
Details: Accurate calculation of water vapor pressure is essential for humidity control, air conditioning design, meteorological studies, and various industrial processes involving air-water vapor mixtures.
Tips: Enter all values in the specified units. Saturation pressure and total pressure should be in Pascals (Pa), while temperatures should be in degrees Celsius (°C). Ensure all values are positive and valid.
Q1: What is the difference between dry bulb and wet bulb temperature?
A: Dry bulb temperature is the air temperature measured by a regular thermometer. Wet bulb temperature is measured by a thermometer with a wet wick around its bulb and indicates the lowest temperature achievable through evaporative cooling.
Q2: How is saturation pressure corresponding to WBT determined?
A: Saturation pressure at wet bulb temperature can be found from steam tables or calculated using empirical formulas that relate temperature to vapor pressure.
Q3: What are typical values for water vapor pressure in atmospheric air?
A: Water vapor pressure in atmospheric air typically ranges from 0 to about 4 kPa, depending on temperature and humidity conditions.
Q4: Why is the denominator in the formula 1544 - 1.44*Tw?
A: This denominator represents an empirical relationship that accounts for the psychrometric constant and the specific heat of moist air, which varies with temperature.
Q5: Can this formula be used for high-temperature applications?
A: The formula is generally valid for typical atmospheric conditions. For high-temperature applications or extreme conditions, more specialized equations may be required.