Degree of Saturation Formula:
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Degree of saturation is the ratio of the volume of water to the volume of voids. It represents how much of the void space in a material is filled with water compared to its maximum capacity.
The calculator uses the Degree of Saturation formula:
Where:
Explanation: The equation calculates the ratio between the actual specific humidity and the maximum specific humidity that the air can hold at a given temperature.
Details: Calculating degree of saturation is crucial for understanding moisture content in materials, predicting weather patterns, and analyzing soil mechanics in geotechnical engineering.
Tips: Enter specific humidity and specific humidity of saturated air values in kg/kg. Both values must be positive and valid for accurate calculation.
Q1: What is the range of degree of saturation values?
A: Degree of saturation ranges from 0 (completely dry) to 1 (fully saturated). Values above 1 indicate supersaturation.
Q2: How is degree of saturation different from relative humidity?
A: While both measure moisture content, degree of saturation relates to volume ratios in materials, while relative humidity relates to partial pressures in air.
Q3: What factors affect degree of saturation?
A: Temperature, pressure, and the material's porosity and permeability affect the degree of saturation.
Q4: Why is degree of saturation important in soil mechanics?
A: It helps determine soil strength, compressibility, and permeability, which are critical for construction and foundation design.
Q5: Can degree of saturation exceed 1?
A: In theory, degree of saturation should not exceed 1, but measurement errors or unusual conditions might produce values slightly above 1.