Specific Gravity Formula:
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Specific Gravity (SG) is a dimensionless unit defined as the ratio of the density of a substance to the density of a reference substance (typically water for liquids and solids). For soils, it helps characterize the material properties and is used in various geotechnical calculations.
The calculator uses the specific gravity formula:
Where:
Explanation: The specific gravity indicates how much denser the soil is compared to water. Typical values for soils range from 2.60 to 2.80.
Details: Specific gravity is used in soil mechanics for void ratio calculations, moisture content determinations, and in the phase relationships of soils. It's essential for classification and understanding soil behavior.
Tips: Enter the measured density of your soil sample in g/cm³. The water density defaults to 1.0 g/cm³ (standard value at 4°C) but can be adjusted for different temperatures if needed.
Q1: What is a typical specific gravity for soils?
A: Most common minerals in soils have specific gravities between 2.60-2.80. Organic soils may have lower values (1.0-2.0).
Q2: Why is water density important in this calculation?
A: Since specific gravity is a ratio, the reference substance's density affects the result. Water density changes slightly with temperature.
Q3: How is soil density measured?
A: Typically using a pycnometer for small samples or sand replacement methods for field measurements.
Q4: Does specific gravity vary with soil moisture?
A: No, specific gravity is a property of the soil solids. However, bulk density (which includes voids) changes with moisture.
Q5: What are the units of specific gravity?
A: Specific gravity is dimensionless since it's a ratio of two densities with the same units.