Boussinesq Vertical Stress Distribution
Computes vertical stress increase Δσz due to surface loading using classical elastic solutions. Choose a load case, enter inputs, and compute stress profile vs depth. Use Load sample to see a ready example.
Inputs
Current units: SI — Q in kN, q in kPa, distances in m, stresses in kPa.
Point load Q at surface, vertical stress at depth z and radial distance r.
Axis stress formula used: Δσz = q [1 − (1 + (R/z)²)^(-3/2)].
Centre stress computed by numerical integration of point-load Boussinesq solution.
Under centre (infinite strip): Δσz = (2q/π) · arctan(B/(2z)).
Summary
Enter inputs and click Compute. Use Load sample to see a complete example.
Results
Boussinesq vertical stress profile
| Depth z | Ratio | Factor | Δσz |
|---|---|---|---|
| No results yet. | |||
Theory & References
Open formulas and references
This tool uses classical elastic half-space solutions (Boussinesq-type). Results are idealized and mainly useful for preliminary checks and understanding stress distribution.
Point load (Boussinesq)
Δσz = (Q / z²) · IB
IB = (3 / 2π) · 1 / (1 + (r/z)²)^(5/2)
Circular UDL (axis)
Δσz = q · [ 1 − (1 + (R/z)²)^(-3/2) ]
Rectangular UDL (centre)
Δσz is computed numerically by integrating point-load Boussinesq solution
over the loaded area (flexible load assumption).
Strip UDL (centre, infinite length)
Δσz = (2q/π) · arctan( B / (2z) )
References
- Boussinesq, J. (1885). Applications des potentiels...
- Poulos & Davis (1974). Elastic Solutions for Soil and Rock Mechanics.
- Das, B.M. Principles of Foundation Engineering (stress distribution chapter).