Specific Gravity Formula:
| From: | To: |
Specific Gravity of Soil is an important property of soil being related to density. It represents the ratio of the density of soil solids to the density of water at a specified temperature.
The calculator uses the Specific Gravity formula:
Where:
Explanation: The formula calculates the specific gravity by considering the dry unit weight of soil, unit weight of water, and the water content at full saturation.
Details: Specific gravity is crucial for determining soil density, void ratio, and degree of saturation. It's essential in geotechnical engineering for soil classification and compaction control.
Tips: Enter dry unit weight in N/m³, unit weight of water in N/m³, and water content as a decimal value. All values must be positive, and water content should be between 0 and 1 for typical soils.
Q1: What is the typical range of specific gravity for soils?
A: Most soils have specific gravity values between 2.60 and 2.80. Organic soils may have values as low as 2.00, while some minerals can have values up to 3.00.
Q2: Why is water content important in specific gravity calculation?
A: Water content affects the density measurement and is necessary to account for the water present in the soil sample during testing.
Q3: What is the standard unit weight of water used in calculations?
A: The standard unit weight of water is 9810 N/m³ (or 9.81 kN/m³) at 4°C, though 1000 kg/m³ density is commonly used.
Q4: How does specific gravity affect soil behavior?
A: Higher specific gravity indicates denser soil particles, which generally means better load-bearing capacity and stability.
Q5: Can this formula be used for all soil types?
A: This formula is generally applicable for most soil types, but special considerations may be needed for organic soils or soils with unusual mineral compositions.