Water Content Formula:
Definition: Water content of soil is the ratio of the mass of water to the total mass of the soil sample, expressed as a percentage.
Purpose: It's a fundamental property in geotechnical engineering that affects soil behavior, strength, and compaction characteristics.
The calculator uses the formula:
Where:
Explanation: The mass of water is divided by the total soil mass, then multiplied by 100 to convert to percentage.
Details: Proper water content measurement is crucial for determining soil compaction, bearing capacity, and settlement characteristics in construction projects.
Tips: Enter the mass of water in kg and total weight of soil in kg. The result will be displayed as a percentage. All values must be ≥ 0, and total weight must be > 0.
Q1: What's a typical water content range for soils?
A: It varies widely: 5-15% for sands, 10-25% for silts, and 20-50% for clays.
Q2: How is mass of water determined in practice?
A: Typically by drying a soil sample and measuring the weight loss (ASTM D2216).
Q3: What's the difference between water content and degree of saturation?
A: Water content is mass ratio, while degree of saturation is volume ratio (how much voids are filled with water).
Q4: Why is water content expressed as percentage?
A: It's a convenient way to express the proportion without units, making comparisons easier.
Q5: How does water content affect soil strength?
A: Generally, strength decreases with increasing water content, especially in fine-grained soils.