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Development of classical bearing capacity theories

Short answer

Rankine (1857) used earth pressure, ignoring width and base friction. Prandtl (1921) added a cohesion term for weightless soil. Reissner (1924) included surcharge. Terzaghi (1943) added soil weight, a rough base, and shape factors, giving qu = cNc + qNq + 0.5γBNγ. Meyerhof, Hansen, and Vesic later introduced depth, shape, inclination, and other correction factors, refining Nγ values.

Explain the development of different classical bearing capacity theories.

Classical bearing capacity theories were developed step by step. Each author added a term that the previous theory neglected.

  1. Rankine (1857) and Bell. Based on Rankine earth pressure. The soil below the footing is in active state and the soil beside it in passive state. For cohesionless soil qu=γDf(1+sin⁡ϕ1−sin⁡ϕ)2q_u = \gamma D_f\left(\dfrac{1+\sin\phi}{1-\sin\phi}\right)^2. Bell (1915) extended it to cc–ϕ\phi soil: qu=γDfNϕ2+2cNϕ(Nϕ+1)q_u = \gamma D_f N_\phi^2 + 2c\sqrt{N_\phi}(N_\phi + 1) with Nϕ=tan⁡2(45∘+ϕ/2)N_\phi = \tan^2(45^\circ + \phi/2). Pauker's method is a similar approach for cohesionless soil. These ignore footing width and base friction.
  2. Prandtl (1921). Studied punching of a rigid die into a weightless cc–ϕ\phi medium. Found a failure surface with a wedge, a log-spiral fan and a passive zone, giving qu=cNcq_u = cN_c with Nc=(Nq−1)cot⁡ϕN_c = (N_q - 1)\cot\phi and Nq=eπtan⁡ϕtan⁡2(45∘+ϕ/2)N_q = e^{\pi\tan\phi}\tan^2(45^\circ + \phi/2). The footing is on the surface and soil is weightless.
  3. Reissner (1924). Extended Prandtl to include the surcharge q=γDfq = \gamma D_f, adding the NqN_q term.
  4. Terzaghi (1943). Added the weight of soil (NγN_\gamma term), a rough base and the effect of shape (square, circular), and gave qu=cNc+qNq+0.5γBNγq_u = cN_c + qN_q + 0.5\gamma BN_\gamma.
  5. Meyerhof (1951, 1963). Included the shear strength of soil above the base, and gave shape, depth and inclination factors.
  6. Hansen (1970) and Vesic (1973). Further refined the factors for shape, depth, inclination of load, base and ground tilt, with improved values of NγN_\gamma.

So the progression is: Rankine (weight and surcharge, approximate) → Prandtl (cohesion) → Reissner (surcharge) → Terzaghi (soil weight, practical form) → Meyerhof, Hansen, Vesic (general equation with correction factors).

✓ Answer checked by Claude Sonnet 5.5

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