Soil Density Formula:
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Definition: Soil density (ρ) is the mass of soil per unit volume, typically measured in kilograms per cubic meter (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 determine its density.
Details: Soil density typically ranges between 1500–2000 kg/m³, varying by soil type:
Tips: Enter the mass of soil in kilograms and volume in cubic meters. Both values must be > 0.
Q1: Why is soil density important?
A: It affects bearing capacity, compaction, water retention, and plant growth in agricultural applications.
Q2: How do I measure soil volume accurately?
A: Use a container with known volume, or for field measurements, use water displacement methods.
Q3: What's the difference between bulk density and particle density?
A: Bulk density includes pore spaces, while particle density measures only the solid particles.
Q4: How does moisture affect soil density?
A: Water increases mass but may slightly increase volume, with net effect depending on soil type.
Q5: What's a good density for construction projects?
A: Typically 1800-2000 kg/m³ after compaction, but requirements vary by project specifications.