Overview
Engineering reference data for Salt Humidity in air psychrometrics.
Key Formulas
Humidity Ratio
Mass of water vapor per mass of dry air.
Relative Humidity
Ratio of actual to saturation vapor pressure.
Wet Bulb Temperature
Temperature measured by wet-bulb thermometer.
Enthalpy of Moist Air
Sensible + latent heat per unit mass of dry air.
Variables
| Symbol | Description | Unit |
|---|---|---|
| Humidity ratio | kg/kg | |
| Relative humidity | % | |
| Vapor pressure | Pa | |
| Saturation vapor pressure | Pa | |
| Dry bulb temperature | °C | |
| Wet bulb temperature | °C |
Data Table: Saturated Salt Solutions for Humidity Control
Properties and Calibration Notes
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Calibration Use: Saturated aqueous solutions of inorganic salts provide a convenient and reliable method for calibrating instruments that measure relative humidity. Each salt establishes a specific, stable humidity level at a given temperature within a sealed container.
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Temperature Dependence: The equilibrium relative humidity is highly sensitive to temperature. Precise temperature control (±0.5°C or better) is critical for accurate calibration, especially for salts with steep humidity-temperature curves.
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Preparation: A saturated solution is a slushy mixture of distilled water and a chemically pure salt. The solution must be saturated (excess solid salt present) and given sufficient time (often 24+ hours) to reach equilibrium before use.
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Important Considerations:
- Accuracy: The tabulated values are theoretical and can vary by several percent in practice due to factors like incomplete saturation, salt impurities, or dissolved gases.
- Common Salts: Sodium chloride (NaCl) is one of the most common references, maintaining ~75% RH near room temperature. Lithium chloride (LiCl) is used for very low humidity (~11% RH).
- Stability: The generated humidity is stable as long as temperature is constant and excess solid salt is present.