This calculator computes the volume and weight relationships in soils, which are useful relationships used in soil mechanics.
Calculation
- Unit weight of water, kN/m3
- Weight of air is zero, therefore
- The calculator assumes the known parameters are the soil sample mass , the over-dry soil sample mass , the volume of the soil sample (based on the test tube dimensions) and soil specific gravity (determined from lab tests). This is a typical situation.
Input
Output
Weight-volume relationships:
Explanation
Weight-Volume Relationships
A soil mass with total volume and total weight is shown below with its three phases of soil mass (soil solids, air and water). Soil mass and it's three phases [Adapted from Source] In most cases you will know the soil sample mass , the over-dry soil sample mass , the volume of the soil sample (based on the test tube dimensions) and soil specific gravity (determined from lab tests). 👉Note, you can either work in mass (with units ) or weight (with units ). If you work in mass, your densities will be in while if you work in weight, your densities will be in . Remember also if you use mass, take and if you use weight, take . We can then determine the remaining mass and volume quantities:
- Volume of soil solids, which is derived using the definition of solid unit weight and the definition of soil specific gravity, . Therefore,
γs=Ms/Vs→Gγw=Ms/Vs→Vs=Ms/Gγw
👉Note, is typically within the range 2.65 (average from granular soils) and 2.80 (average for cohesive soils). - Volume of voids,
- Volume of water,
- Volume of air,
We now know all our mass and volume quantities (). We can then define the following weight-volume relationships commonly used in soil mechanics: - Void ratio,
- Porosity,
- Degree of saturation, which can range between zero for a completely dry soil, to 1 for a fully saturated soil
- Moisture content,
- Unit weight, , also known as moist unit weight or total unit weight since it includes weight of water and soil solids
- Dry unit weight,
- Solid unit weight,
- Saturated unit weight, for (i.e. ) is when the soil is completely saturated
- Submerged (buoyant) unit weight, for is when the soil is below the ground water table
Weight-Volume Relationships for
Useful weight-volume relationships can be developed by considering a soil sample with as shown below. Therefore, the volume of voids . Weight-volume relationships for [Adapted from Source] Weight-volume relationships can then be derived in terms of . Here are some common forms: - Moist unit weight,
- Dry unit weight,
- Degree of saturation,
- Saturated unit weight,
- Submerged unit weight,
Weight-Volume Relationships for
Useful weight-volume relationships can also be developed by considering a soil sample with as shown below. Therefore, the volume of voids . Weight-volume relationships for [Adapted from Source] Weight-volume relationships can then be derived in terms of . Here are some common forms: - Moist unit weight,
- Dry unit weight,
- Saturated unit weight,
References
- Advanced Soil Mechanics by Braja M. Das
- Soil Phase Diagram and Relationship Formulas
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