18-Env-A3 Geotechnical and Hydrogeological Engineering · December 2016
Question 3 of 6: Differential Settlement of Two Foundations on a Variable-Thickness Clay
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
Notes on this paper
National Exams — December 2016 — 04-Env-A3 / Geotechnical & Hydrogeological Engineering. 3 hours duration; open book exam, any non-communicating calculator permitted. FIVE (5) questions constitute a complete exam paper (the first five as they appear in the answer book are marked, 20 marks each, 100 marks total); all six printed questions are solved below for completeness.
Reference texts. Braja M. Das, Principles of Geotechnical Engineering (9th ed.) — weight–volume relations, permeability, seepage/flow nets, stress distribution, consolidation and lateral earth pressure chapters; Craig & Knappett, Craig's Soil Mechanics (8th ed.) — cross-reference for seepage, flow nets and anchored sheet-pile wall design.
Question 3: Differential Settlement of Two Foundations on a Variable-Thickness Clay (20 marks)
Given. Two identical 1.5 m × 1.5 m footings, each carrying 780 kN, founded on sand over a clay wedge (1.2 m thick under Foundation A, 2.8 m thick under Foundation B) over gravel.
Given data
Quantity
Symbol
Value
Column load (each footing)
$P$
780 kN
Footing size
$B\times L$
1.5 m × 1.5 m
Sand above clay, under A / B
—
3.0 m / 1.4 m
Clay thickness, under A / B
$H_A,\,H_B$
1.2 m / 2.8 m
Clay compressibility
$m_v$
0.7 m²/MN
Observed differential settlement at $t=2$ yr
—
10 mm
Jamming threshold
—
24 mm
Find. (a) the ultimate (expected total) differential settlement between A and B; (b) how much longer until the differential settlement reaches 24 mm.
Figure 2 — the two footings and the wedge-shaped clay layer revealed by the follow-up investigation.
Approach. Each footing's own clay settlement is $S=m_v\,\Delta\sigma_z\,H$, where $\Delta\sigma_z$ is the Boussinesq stress increase at the clay's mid-depth under the CENTRE of that footing (found by superposing four quarter-rectangle corner solutions) and $H$ is the clay thickness beneath that footing. The difference $S_A-S_B$ is the ultimate differential settlement; scaling that ultimate value by Terzaghi's average degree-of-consolidation curve $U(T_v)$, calibrated against the one observed data point (10 mm at 2 years), gives the time to reach any other differential settlement, since $T_v\propto t$ for fixed $c_v$ and drainage path.
Footing pressure. $q=P/(B L)=780/(1.5\times1.5)=346.7$ kPa (identical for A and B).
Stress increase at each clay mid-depth (Boussinesq, under footing centre). Mid-clay depths are $z_A=3.0+1.2/2=3.6$ m and $z_B=1.4+2.8/2=2.8$ m below the footing base. Superposing four $0.75\times0.75$ m corner solutions,
$$\Delta\sigma_A=4qI(m,n)\Big|_{z=3.6}=\boxed{26.8\ \text{kPa}},\qquad \Delta\sigma_B=4qI(m,n)\Big|_{z=2.8}=\boxed{42.4\ \text{kPa}}.$$
(The influence factor $I$ is evaluated from the standard Newmark corner-of-rectangle formula.)
Ultimate settlement of each footing.
$$S_A=m_v\Delta\sigma_A H_A=0.7\times10^{-3}\times26.8\times1.2\times1000=\boxed{22.5\ \text{mm}},$$
$$S_B=m_v\Delta\sigma_B H_B=0.7\times10^{-3}\times42.4\times2.8\times1000=\boxed{83.1\ \text{mm}}.$$
Part (a) — ultimate differential settlement.
$$\Delta S_{ult}=S_B-S_A=83.1-22.5=\boxed{60.6\ \text{mm}}.$$
Part (b) — calibrate the consolidation-rate curve. The observed 10 mm at $t=2$ yr corresponds to an average degree of consolidation $U_1=10/60.6=16.5\%$, giving (from $T_v=\tfrac{\pi}{4}U^2$ for $U\le60\%$) $T_{v,1}=0.0214$. The 24 mm jamming threshold needs $U_2=24/60.6=39.6\%$, giving $T_{v,2}=0.123$.
Solve for the required elapsed time. Since $T_v=c_v t/d^2\propto t$ for the same soil and drainage path, $t_2=t_1\,T_{v,2}/T_{v,1}=2\times(0.123/0.0214)=\boxed{11.5\ \text{years since construction}}$, i.e. a further $t_2-2=\boxed{9.5\ \text{years (≈114 months) from today}}$.
Check: part (b) assumes the differential settlement follows the SAME dimensionless consolidation-rate curve as the ultimate settlement (a single effective $c_v$/drainage path for the site), calibrated from the one observed differential-settlement–time data point given — the only approach the given data supports, since $c_v$ itself is not stated.