Angle of Internal Friction Formula:
Definition: The angle of internal friction (φ) is a measure of the shear strength of soil due to friction between soil particles.
Purpose: It's a critical parameter in geotechnical engineering for analyzing slope stability, bearing capacity, and earth pressure calculations.
The calculator uses the formula:
Where:
Explanation: The formula calculates the angle by considering the balance between resisting forces (from friction and cohesion) and driving forces.
Details: This parameter helps determine:
Tips:
Q1: What's a typical range for φ in soils?
A: Sands: 28°-45°; Silts: 25°-35°; Clays: 10°-25° (can be 0° for pure soft clay).
Q2: How does cohesion affect the calculation?
A: Cohesion provides additional shear strength independent of normal stress.
Q3: What if I get a negative angle result?
A: Check your inputs - this suggests the resisting moment is insufficient for the given cohesion and normal forces.
Q4: Why include a tolerance range?
A: Soil properties are naturally variable - the range accounts for potential measurement and estimation uncertainties.
Q5: How is this different from the friction angle in direct shear tests?
A: This calculates the effective friction angle considering the entire failure surface, while direct shear gives the peak friction angle for a specific sample.