Formula Used:
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Water Content of Soil from Pycnometer is the ratio of the weight of water to the weight of the solids in a given mass of soil. It is a fundamental parameter in soil mechanics and geotechnical engineering.
The calculator uses the formula:
Where:
Explanation: This formula calculates the water content based on the degree of saturation, specific gravity of soil, unit weight of water, and dry unit weight of the soil.
Details: Accurate water content calculation is crucial for determining soil properties, assessing soil stability, and designing foundations and earthworks in geotechnical engineering.
Tips: Enter all values with appropriate units. Degree of Saturation, Specific Gravity, Unit Weight of Water, and Dry Unit Weight must be positive values.
Q1: What is the typical range for water content in soils?
A: Water content can vary widely from near 0% for dry soils to over 100% for highly saturated clays and organic soils.
Q2: How does water content affect soil behavior?
A: Water content significantly influences soil strength, compressibility, permeability, and compaction characteristics.
Q3: What is the pycnometer method?
A: The pycnometer method is a laboratory technique used to determine specific gravity of soil solids and water content using a calibrated flask.
Q4: Why is unit weight of water typically 9810 N/m³?
A: 9810 N/m³ is the unit weight of water at standard conditions (4°C), calculated as density (1000 kg/m³) multiplied by gravity (9.81 m/s²).
Q5: What are the limitations of this calculation?
A: This calculation assumes homogeneous soil properties and may not account for soil fabric, temperature variations, or the presence of organic matter.