Degree Of Saturation Given Relative Humidity Formula:
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Degree of saturation is the ratio of the volume of water to the volume of voids in a soil or air mixture. It indicates how much of the void space is filled with water compared to the maximum possible amount.
The calculator uses the Degree of Saturation formula:
Where:
Explanation: The formula calculates the degree of saturation based on relative humidity and pressure relationships in moist air.
Details: Calculating degree of saturation is important in soil mechanics, geotechnical engineering, and atmospheric sciences to understand moisture content and air-water relationships in various materials and environments.
Tips: Enter relative humidity as a decimal between 0 and 1, partial pressure and total pressure in Pascals. Ensure partial pressure is less than or equal to total pressure.
Q1: What is the difference between degree of saturation and relative humidity?
A: Relative humidity measures air moisture content relative to maximum capacity at a given temperature, while degree of saturation specifically measures the ratio of water volume to void volume.
Q2: What are typical values for degree of saturation?
A: Degree of saturation ranges from 0 (completely dry) to 1 (completely saturated). Most natural soils have values between 0.2 and 0.9.
Q3: How is partial pressure of water vapour determined?
A: Partial pressure of water vapour in saturated air is obtained from steam tables corresponding to the dry bulb temperature of the air.
Q4: What units should be used for pressure values?
A: While Pascals are used in this calculator, consistent pressure units can be used as long as both partial pressure and total pressure use the same units.
Q5: When is this calculation most useful?
A: This calculation is particularly useful in geotechnical engineering for soil analysis and in HVAC systems for moisture control calculations.