16-Civ-B3 Geotechnical Design · May 2015
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
Paper format. Professional Engineers Ontario / Engineers Canada National Examinations, May 2015 — 98-Civ-B3 Geotechnical Design. Three hours, OPEN BOOK, any non-communicating calculator. Section A carries five discussion questions of 7 marks each (answer any four); Section B carries four design questions of 24 marks each (answer any three); the examinable total is 4 × 7 + 3 × 24 = 100 marks. All nine questions are worked below, because the set is a study resource rather than a timed attempt.
Reference texts (98-Civ-B3 / 16-Civ-B3 Geotechnical Design).
Sources of design charts and assumed values (page-1 Note 6). Note 6 of this paper requires the candidate to identify the source of every design chart used and of every value assumed in the absence of data. They are named where used and collected here:
Question text not reproduced: the examination questions are © Engineers and Geoscientists BC. Open the official past paper (linked at the top of this page) to read the question, then follow the worked solution below.
The observation is the empirical basis of the alpha method, in which the limiting unit shaft resistance in a clay is written $f_s = \alpha\,c_u$. Back-analysis of load tests gives $\alpha \approx 1.0$ for soft normally consolidated clays ($c_u \lesssim 50$ kPa) but $\alpha \approx 0.3$ to $0.5$ for stiff overconsolidated clays. The reasons are all consequences of what pile installation does to the soil immediately around the shaft, and of what the shaft-soil interface can subsequently recover.
Installation disturbance and reconsolidation. Driving a displacement pile completely remoulds an annulus of clay one to two diameters thick and generates large excess pore pressures. In a soft, normally consolidated clay this excess pore pressure dissipates radially over weeks to months, the remoulded annulus reconsolidates against the pile, and the horizontal effective stress on the shaft returns to something close to, or even above, its pre-driving value. Because a soft clay is only lightly structured, remoulding destroys little strength that reconsolidation and thixotropic regain do not restore; the shaft therefore ends up with an interface strength close to the intact $c_u$, hence $\alpha \approx 1$. In a stiff overconsolidated clay the same driving process is far more damaging: the clay is strongly structured, often cemented and always fissured, and remoulding at large strain destroys a bonding that reconsolidation cannot rebuild.
Negative pore pressures and softening. Shearing a heavily overconsolidated clay is dilatant, so driving generates negative excess pore pressures near the shaft. As those negative pressures dissipate, water migrates toward the pile and the annulus softens — its water content rises and its undrained strength falls permanently. The long-term shaft resistance is therefore governed by a softened, near-normally-consolidated material, not by the stiff intact clay from which $c_u$ was measured.
The gap, and the mismatch of stress level. A stiff clay stands unsupported, so a driven or bored pile in stiff clay commonly leaves an open annular gap over the upper several diameters, or a slurry-smeared, low-strength film in the case of a bored pile; over that length the shaft resistance is essentially zero. More fundamentally, the shaft resistance is really an effective-stress phenomenon, $f_s = \beta\,\sigma'_v = K\tan\delta\,\sigma'_v$. A stiff clay owes its high $c_u$ to a past overburden that no longer exists, so the current vertical effective stress is modest while $c_u$ is large; the ratio $f_s/c_u$ must therefore be small. In a soft normally consolidated clay $c_u/\sigma'_v \approx 0.22$ to $0.25$ throughout, so the same effective-stress mechanism produces $f_s$ of the same order as $c_u$.
Brittleness and progressive failure. Finally, a stiff clay is strain-softening: its peak strength is mobilised at small displacement and falls toward a residual value beyond it. A 20 m pile does not slip uniformly — the top of the shaft reaches peak and passes into the softening branch while the toe is still loading elastically — so the peak $c_u$ is never available simultaneously over the full shaft. Soft clay is essentially ductile and does not suffer this progressive-failure loss. For Canadian practice, CFEM 4th ed. Ch. 18 recommends exactly this treatment: $\alpha$ near unity in soft sensitive clays such as the Champlain Sea deposits, with much lower values in the stiff glacial tills and Cretaceous clays of the Prairies, and confirmation by static load test.