Density of Solids Formula:
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Density of Solids (ρs) is the mass of soil solids per unit volume of solids. It represents how much mass is contained within a given volume of solid material, excluding any voids or pores.
The calculator uses the density formula:
Where:
Explanation: The formula converts unit weight (force per unit volume) to density (mass per unit volume) by dividing by gravitational acceleration.
Details: Density of solids is fundamental in geotechnical engineering for soil classification, compaction analysis, and understanding soil behavior under various loading conditions.
Tips: Enter the unit weight of solids in N/m³. The value must be positive and greater than zero for accurate calculation.
Q1: What is the difference between density and unit weight?
A: Density is mass per unit volume (kg/m³), while unit weight is weight (force) per unit volume (N/m³). They are related through gravitational acceleration.
Q2: Why divide by 9.8 specifically?
A: 9.8 m/s² is the standard acceleration due to gravity used to convert between mass and weight (F = m × g).
Q3: What are typical density values for common materials?
A: Typical soil solids density ranges from 2500-2700 kg/m³ for most mineral soils, while organic materials may have lower densities.
Q4: How does this relate to bulk density?
A: Density of solids considers only the solid particles, while bulk density includes both solids and voids in the total volume.
Q5: When is this calculation most important?
A: This calculation is crucial in soil mechanics for determining porosity, void ratio, and other important geotechnical properties.