What is degree of saturation in soil?
Degree of saturation (S) is the percentage of pore space in soil that is filled with water.
How do I calculate degree of saturation?
Use the formula S = (w / Gs * e) * 100%, where w is water content, Gs is specific gravity of solids, and e is void ratio.
Why is degree of saturation important in soil engineering?
It affects soil strength, compressibility, permeability, and the effective stress on the soil skeleton.
What does water content (w) represent in this calculation?
Water content represents the mass of water per unit mass of dry soil.
How is specific gravity of solids (Gs) used in degree of saturation calculations?
Gs relates the density of soil particles to that of water, influencing how much water the soil can hold.
Can degree of saturation be greater than 100%?
No, degree of saturation cannot exceed 100%, as it represents the maximum possible water content in the pores.
What are some common applications for this calculator?
It’s used in civil engineering projects to assess soil conditions, foundation design, and drainage systems.