16-Civ-A4 Geotechnical Materials and Analysis · December 2017
Question 5 of 6: Pore Pressure and Consolidation State from a CU Test
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
Notes on this paper
Paper format: National Examinations — 16-Civ-A4 Geotechnical Materials and Analysis, December 2017.
Closed book, 3 hours, 100 marks. Answer all six questions. Charts (rectangular-area influence chart, Newmark chart) and a formula sheet are provided at the back of the exam.
Reference texts: R.F. Craig & J. Knappett, Craig’s Soil Mechanics (8th ed.); B.M. Das, Principles of Geotechnical Engineering; R.D. Holtz, W.D. Kovacs & T.C. Sheahan, An Introduction to Geotechnical Engineering (2nd ed.); M. Budhu, Soil Mechanics and Foundations.
Question 5: Pore Pressure and Consolidation State from a CU Test (20 marks)
Given. A CU triaxial test with total stresses σ3 = 100 kPa and deviator 60 kPa at failure (so σ1 = 160 kPa), together with the soil’s unique effective envelope (CD): c′ = 0, φ′ = 30°, and the total-stress CU envelope c = 0, φ = 13.3°.
Given data
Confining pressure, σ3
100 kPa (total)
Deviator stress at failure
60 kPa ⇒ σ1 = 160 kPa
Effective (CD) parameters
c′ = 0, φ′ = 30°
Total (CU) parameters
c = 0, φ = 13.3°
Find. The pore-water pressure uw at failure, the Skempton pore-pressure coefficients A and B, and whether the clay is normally or over-consolidated (with three reasons).
Approach. The effective-stress failure envelope is a property of the soil alone, so the CU test’s effective stresses must lie on it; imposing that condition (with c′ = 0) yields uw directly. B follows from saturation and A from the measured pore pressure over the deviator stress.
Effective-stress failure condition. With c′ = 0, at failure $\sigma_1'=\sigma_3'\tan^{2}\!\left(45^\circ+\tfrac{\phi'}{2}\right)$. Here $\tan^{2}(45^\circ+15^\circ)=\tan^{2}60^\circ=3$.
Solve for the pore pressure. Substituting σ′ = σ − uw:
$$(160-u_w)=3\,(100-u_w)\;\Rightarrow\;2u_w=140\;\Rightarrow\;\boxed{u_w=70\ \text{kPa}}.$$
Check: the total-stress angle is $\sin\phi_{cu}=\dfrac{\sigma_1-\sigma_3}{\sigma_1+\sigma_3}=\dfrac{60}{260}=0.231\Rightarrow\phi_{cu}=13.3^\circ$, matching the given CU value.
Coefficient B. The specimen is saturated (a CU test is run on a saturated sample), so
$$B=1.0.$$
Coefficient A. After consolidation under the cell pressure the excess pore pressure is zero, so all of uw is generated by the deviator stage (Δσ3 = 0, Δσd = 60):
$$A_f=\frac{\Delta u}{\Delta\sigma_d}=\frac{70}{60}=\boxed{1.17}.$$
Consolidation state. Three consistent indicators show the clay is normally consolidated: (i) the effective envelope passes through the origin (c′ = 0); (ii) large positive pore pressure at failure with Af = 1.17 > 0.5, i.e. strongly contractive behaviour; (iii) the CU total-stress angle (13.3°) is far below φ′ (30°), the signature of positive shear-induced pore pressure. (An over-consolidated clay would show c′ > 0, Af near or below zero, and even negative pore pressure.)
Results
Quantity
Value
Pore-water pressure at failure, uw
70 kPa
Skempton B
1.0 (saturated)
Skempton Af
1.17
Consolidation state
Normally consolidated
The result illustrates why the drained (CD) parameters c′, φ′ — not the total-stress CU angle — are the correct inputs for long-term (drained) stability analyses such as the earth-dam problem in Question 1(8): the CU total angle understates the true frictional resistance precisely because of the positive pore pressure quantified here.