Bulk Density Formula:
Definition: Bulk density is the ratio of total mass of soil to its total volume, including both solids and pore spaces.
Purpose: It's a fundamental property in soil mechanics that affects water movement, root penetration, and nutrient availability.
The calculator uses the formula:
Where:
Explanation: The total soil weight is divided by the total volume it occupies to determine its bulk density.
Details: Bulk density indicates soil compaction and porosity. Higher values suggest more compacted soil with less pore space.
Tips: Enter the total weight of soil in kg and total volume in m³. The ±5% indicates typical measurement accuracy ranges.
Q1: What's a typical bulk density range for soils?
A: Most mineral soils range from 1.1-1.6 g/cm³ (1100-1600 kg/m³), while organic soils are lower (0.2-0.8 g/cm³).
Q2: Why include ±5% in measurements?
A: This accounts for typical measurement errors in field conditions when collecting soil samples.
Q3: How is total volume measured?
A: Typically using core sampling methods where a known volume of soil is extracted and weighed.
Q4: What affects bulk density?
A: Soil texture, organic matter content, compaction, and moisture content all influence bulk density.
Q5: How does bulk density relate to porosity?
A: Higher bulk density generally means lower porosity as there's less space between soil particles.