GEO-21
Vesic bearing capacity
qult = c Nc sc dc + q Nq sq dq + ½ γ B Nγ sγ dγ. Shape and depth factors on Terzaghi's three terms.
Governing equation
where
- c'
- Cohesion (kPa)
- N_c
- Nc (—)
- N_q
- Nq (—)
- N_\gamma
- Nγ (—)
- q
- Overburden q (kPa)
- \gamma
- Unit weight (kN/m³)
- B
- Width (m)
- s_c
- Shape sc (—)
- s_q
- Shape sq (—)
- s_\gamma
- Shape sγ (—)
- d_c
- Depth dc (—)
- d_q
- Depth dq (—)
- d_\gamma
- Depth dγ (—)
- q_{ult}
- Ultimate bearing (kPa)
Lecture brief
Historical brief
Soil mechanics became a quantitative laboratory after Karl von Terzaghi’s 1925–1943 work on effective stress, consolidation and bearing. These sheets still size shallow foundations, retaining walls, piles and drainage in SI. This sheet (GEO-21 — Vesic bearing capacity) is the form associated with Vesic 1975. Working symbols: , , , , , , , , , , , , . Vesic recast Prandtl–Reissner with rigidity Ir and shape sc, sq, sγ plus depth dc, dq, dγ.
Purpose
Live realistic example
In symbols
Calculator
Inputs
Outputs
- Ultimate bearing q_{ult}1556.3 kPa
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Narration of this film
A footing, three capacity bars scaled by shape and embedment.
Vesic recast Prandtl–Reissner with rigidity Ir and shape sc, sq, sγ plus depth dc, dq, dγ.
Watch on YouTube