This post presents a solved example on elastic settlement of shallow foundations. Foundation settlement is mainly made up of elastic (or immediate) settlement, Se, and consolidation settlement, Sc. Immediate settlement takes place as the load is applied, or within a time period of about 7 days. It is used for all fine-grained soils including silts and clays with a degree of saturation less than or approximately less than 90%, and for all coarse-grained soils with a large coefficient of permeability, say above 10-3 m/s.
To assess immediate settlement of a shallow foundation, it is imperative to obtain reliable values of elastic parameters of the soil. Values from laboratory can contain errors of about 50%, and in-situ tests are often more preferred, with close attention being paid to the anisotropic behaviour of soils. A range of values can be seen from the Table below;
It is also necessary to obtain a reliable stress profile from the applied load. We normally have the problem of computing both correct numerical values and the effective depth H of the influence zone. Theory of elasticity equations are used for the stress computation, with the influence depth (H) below the loaded area taken as H = 0, to H = ∞.
However, note that the stratum depth actually causing settlement is not at H/B = ∞, but is at any of the following;
(a) Depth (z) = 5B; where B is the least total lateral dimension of the footing
(b) Depth to where a hard stratum is encountered. Take hard as that stratum where the modulus of elasticity is ten times the modulus of elasticity of the upper layer.
The equation for computing the elastic settlement of a shallow footing is as given below;
qo = net applied pressure on the foundation
μs = Poisson’s ratio of soil
ES = Average modulus of elasticity of the soil under the foundation from z = 0 to about z = 4B or 5B
Due to the non-homogeneous nature of soil deposits, the magnitude of Es may vary with depth. For that reason, Bowles (1987) recommended using a weighted average value of Es as given in the equation (2) below;
ES(i) = Soil modulus of elasticity within a depth ∆z
z ̅ = H or 5B, whichever is smaller
B’ = B/2 for centre of foundation, B for corner of foundation
IS = Shape factor according to Steinbrenner (1934)
If = Depth factor which depends on (Df/B, μs, L/B)
Charts for computing If are available in standard geotechnical engineering textbooks.
α = factor that depends on the location on the foundation where settlement is being calculated
For calculation of settlement at the centre of the foundation;
α = 4; m’= L/B; n’ = H/0.5B
For calculation of settlement at the corner of the foundation;
α = 1; m’= L/B; n’ = H/B
For the example given below, compute the settlement at the centre of the footing, assuming that a net pressure of 145 KN/m2 is exerted by the foundation.
Given that B = 1.8m, L = 2.7m; z ̅ = (5 × 1.8) = 9.0 m = H (9.0 m)
Es = [12000(5) + 7500(3) + 10200(1.2)] / 9 = 10526.667 KN/m2
At the centre of the foundation;
α = 4; m’= L/B =2.7/1.8 =1.5 ; n’ = H/0.5B=9/(0.5(1.8)) = 10
A0 = 1.5 In ((1+ (1.52 + 1)0.5) × (1.52 + 102)) / 1.5 (1 + (1.52+ 102 + 1)0.5)
= 1.5 In(2.803 × 10.112) / (1.5 × 11.161) = 0.7896
A1 = In ((1.5 + (1.52 + 1)) × (1 + 102)) / (1.5 + (1.52 + 102 + 1)0.5)
= In[(3.3027 × 10.049) / (1.5 + 10.161)] = 1.0459
A2 = 1.5 / [10 (1.52 + 102 + 1)0.5] = 1.5 / (10 × 10.161) = 0.0147
F1 = 1/π (A0 + A1 ) = 1/π (0.7896 + 1.0459) = 0.5842
F2 = (n’/2π) tan-1A2 = 10/2π tan-1(0.0147) = 0.0233 (calculated in radians)
Therefore, the shape factor according to Steinbrenner;
IS = F1 + [(1 – 2μs)/(1 – μs)] × F2 = 0.5842 + [(1 – (2 × 0.3) / (1 – 0.3)] × 0.0233 = 0.5975
From chart, let us obtain the foundation embedment factor (If);
Df/B = 0.9/1.8 = 0.5
L/B = 2.7/1.8 = 1.5
From the chart, say If = 0.79
Inputting all the parameters into the elastic settlement equation given in (1)
Se = qo α × B’ × ((1- μs2)/Es) × Is × If
Se = 145 × 4 × 0.9 × ((1 – 0.32)/10526.667) × 0.5975 × 0.79 = 0.0213m = 21.3 mm
This gives the elastic settlement at the centre of the footing. A lot of modifications and other proposals have been made by scholars over years due to improved research, and we will keep posting them as time goes on.
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