Soil Density Formula:
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Definition: Soil density (ρ) is the mass of soil per unit volume, typically expressed in kg/m³.
Purpose: Understanding soil density is crucial for construction, agriculture, and environmental engineering projects.
The calculator uses the formula:
Where:
Explanation: The mass of soil is divided by its volume to calculate its density.
Details: Soil density affects load-bearing capacity, water retention, and root penetration in agricultural applications.
Tips: Enter the mass of soil in kilograms and volume in cubic meters. Both values must be > 0.
Q1: What's a typical soil density range?
A: Most soils range from 1,000 to 2,000 kg/m³, with clay soils typically denser than sandy soils.
Q2: How do I measure soil mass?
A: Use a scale to weigh a known volume of soil after drying to remove moisture.
Q3: How do I measure soil volume?
A: For loose soil, use a container of known volume. For in-situ measurements, use displacement methods.
Q4: What's bulk density vs particle density?
A: Bulk density includes pore spaces, while particle density measures only the solid particles.
Q5: Why does soil density matter in construction?
A: It determines bearing capacity and settlement characteristics for foundations.