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Total Volume Of Soil Given Dry Unit Weight Of Soil Calculator

Formula Used:

\[ V = \frac{W_s}{\rho_d} \]

kg
kg/m³

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1. What is Total Volume in Soil Mechanics?

Total Volume in Soil Mechanics is defined as the total capacity of the soil sample, representing the space occupied by both solid particles and voids. It is a fundamental parameter in geotechnical engineering calculations.

2. How Does the Calculator Work?

The calculator uses the formula:

\[ V = \frac{W_s}{\rho_d} \]

Where:

Explanation: This formula calculates the total volume by dividing the weight of solid particles by the dry density of the soil.

3. Importance of Volume Calculation

Details: Accurate volume calculation is essential for determining soil properties, designing foundations, calculating earthwork quantities, and assessing soil compaction in construction projects.

4. Using the Calculator

Tips: Enter weight of solids in kilograms and dry density in kg/m³. Both values must be positive numbers greater than zero for accurate calculation.

5. Frequently Asked Questions (FAQ)

Q1: What is the difference between total volume and solid volume?
A: Total volume includes both solid particles and void spaces, while solid volume refers only to the space occupied by the solid particles themselves.

Q2: How is dry density different from bulk density?
A: Dry density considers only the mass of solids per unit volume, while bulk density includes the mass of both solids and water present in the soil.

Q3: When should this calculation be used?
A: This calculation is particularly useful in soil compaction testing, earthwork calculations, and when determining the volume of soil required or removed in construction projects.

Q4: What are typical dry density values for different soil types?
A: Dry density varies by soil type: sands (1500-1800 kg/m³), silts (1300-1600 kg/m³), clays (1100-1500 kg/m³), depending on compaction and moisture content.

Q5: How does moisture content affect this calculation?
A: This calculation uses dry density, which already accounts for the absence of water. For wet soils, the dry density must be determined by drying the soil sample first.

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