INGENIA

GEO-22

Hansen bearing capacity

qult = c Nc sc dc ic + q Nq sq dq iq + ½ γ B Nγ sγ dγ iγ. Inclination cuts the Nγ term hardest.

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BearingHansen 1970

Governing equation

qult=cNcscdcic+qNqsqdqiq+12γBNγsγdγiγq_{ult}=c N_c s_c d_c i_c+q N_q s_q d_q i_q+\tfrac12\gamma B N_\gamma s_\gamma d_\gamma i_\gamma

ic∈[0.3,1]i_c \in \left[0.3, 1\right]

where

c'
Cohesion (kPa)
N_c
Nc (—)
N_q
Nq (—)
N_\gamma
Nγ (—)
q
Overburden (kPa)
\gamma
Unit weight (kN/m³)
B
Width (m)
i_c
Inclination ic (—)
i_q
Inclination iq (—)
i_\gamma
Inclination iγ (—)
q_{ult}
Ultimate bearing (kPa)

The figure, part by part

Each numbered marker wears the color of its card. Hover a card to light the marker. Tap a marker to jump to that card. The slider walks a red point along the curve; Animate drawing traces it like a pen.

GEO-22 · bearing
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①

Governing law — red

qult=cNcscdcic+qNqsqdqiq+12γBNγsγdγiγq_{ult}=c N_c s_c d_c i_c+q N_q s_q d_q i_q+\tfrac12\gamma B N_\gamma s_\gamma d_\gamma i_\gamma

ic∈[0.3,1]i_c \in \left[0.3, 1\right]

ic=0.3i_c = 0.3qult=606.2q_{ult} = 606.2

②

Domain of the variable — blue

i_c_{\min} = 0.3,\quad i_c_{\max} = 1

ic∈[0.3,1]i_c \in \left[0.3, 1\right]

ic=0.3i_c = 0.3ic=0.3i_c = 0.3

③

Response curve — green

qult=cNcscdcic+qNqsqdqiq+12γBNγsγdγiγq_{ult}=c N_c s_c d_c i_c+q N_q s_q d_q i_q+\tfrac12\gamma B N_\gamma s_\gamma d_\gamma i_\gamma

ic∈[0.3,1]i_c \in \left[0.3, 1\right]

ic=0.3i_c = 0.3qult=606.2q_{ult} = 606.2

④

Rate of change — amber

dqultdic\frac{\mathrm{d}q_{ult}}{\mathrm{d}i_c}

ic∈[0.3,1]i_c \in \left[0.3, 1\right]

ic=0.304i_c = 0.304qult′=363q_{ult}^{\prime} = 363

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-22 — Hansen bearing capacity) is the form associated with Hansen 1970. Working symbols: c′c', NcN_c, NqN_q, NγN_\gamma, qq, γ\gamma, BB, ici_c, iqi_q, iγi_\gamma →\rightarrow qultq_{ult}. Hansen added load inclination, base tilt and ground slope to Brinch Hansen's general formula.

Purpose

Purpose: compute qultq_{ult} from c′c', NcN_c, NqN_q, NγN_\gamma, qq, γ\gamma, BB, ici_c, iqi_q, iγi_\gamma in Geotechnical engineering via qult=cNcscdcic+qNqsqdqiq+12γBNγsγdγiγq_{ult}=c N_c s_c d_c i_c+q N_q s_q d_q i_q+\tfrac12\gamma B N_\gamma s_\gamma d_\gamma i_\gamma qult = c Nc sc dc ic + q Nq sq dq iq + ½ γ B Nγ sγ dγ iγ. Inclination cuts the Nγ term hardest. Use it when a real geotechnical engineering question must be answered in SI before a code check.

Live realistic example

In symbols

Live case. Given c′=12.000 kPac' = 12.000\,\mathrm{kPa}, Nc=25.000 —N_c = 25.000\,\mathrm{—}, Nq=12.000 —N_q = 12.000\,\mathrm{—}, Nγ=10.000 —N_\gamma = 10.000\,\mathrm{—}, q=30.000 kPaq = 30.000\,\mathrm{kPa}, γ=18.000 kN/m3\gamma = 18.000\,\mathrm{kN/m^{3}}, B=2.500 mB = 2.500\,\mathrm{m}, ic=0.850 —i_c = 0.850\,\mathrm{—}, iq=0.800 —i_q = 0.800\,\mathrm{—}, iγ=0.700 —i_\gamma = 0.700\,\mathrm{—}, the governing relation qult=cNcscdcic+qNqsqdqiq+12γBNγsγdγiγq_{ult}=c N_c s_c d_c i_c+q N_q s_q d_q i_q+\tfrac12\gamma B N_\gamma s_\gamma d_\gamma i_\gamma yields qult=805.9 kPaq_{ult} = 805.9\,\mathrm{kPa}. A tilted load on a strip, three reduced capacity bars. Move a slider: the numbers are this situation, not a canned story.

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  • Ultimate bearing q_{ult}805.9 kPa
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GEO-22 · bearing
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Narration of this film

A tilted load on a strip, three reduced capacity bars.

Hansen added load inclination, base tilt and ground slope to Brinch Hansen's general formula.

Reading speed

Watch on YouTube