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.
Given.
| Quantity | Symbol | Value |
|---|---|---|
| Footing plan dimensions | $B \times L$ | 1.5 m $\times$ 2.5 m |
| Column load | $Q$ | 120 kN |
| Depth of footing base | $D_f$ | 1.5 m |
| Upper sand, 0 to 1.5 m (moist) | $\gamma$ | 15 kN/m$^3$ |
| Lower sand, 1.5 to 3.0 m (saturated) | $\gamma_{sat}$ | 18 kN/m$^3$ |
| Groundwater table depth | $d_w$ | 1.5 m |
| Clay layer, 3.0 to 5.5 m | $H_c$ | 2.5 m |
| Clay water content / specific gravity / liquid limit | $w,\ G_s,\ LL$ | 35 per cent, 2.7, 38 |
Find. The primary consolidation settlement of the normally consolidated clay layer under the footing load, plus two alternative methods for the same calculation and the extra data each of them needs.
[Figure not reproduced: Figure 2 (redrawn) — footing at 1.5 m depth over 1.5 m of saturated sand and a 2.5 m normally consolidated clay layer. The settlement is computed at the top, middle and bottom of the clay and combined by the weighted average the paper prescribes. See the official exam paper.]
Approach. Establish the clay's index properties from $w$ and $G_s$, compute the existing effective overburden at mid-clay, distribute the foundation pressure to the top, middle and bottom of the clay with the 2:1 method, combine them with the weighted average given in the question, and apply the one-dimensional normally consolidated compression equation.
| Quantity | Value |
|---|---|
| Contact pressure, $q$ | 32.0 kPa |
| Initial void ratio, $e_0 = wG_s$ | 0.945 |
| Clay saturated / submerged unit weight | 18.38 / 8.57 kN/m$^3$ |
| Effective overburden at mid-clay, $\sigma'_0$ | 45.50 kPa |
| $\Delta\sigma'_t$ / $\Delta\sigma'_m$ / $\Delta\sigma'_b$ (2:1) | 10.00 / 5.38 / 3.36 kPa |
| Weighted average, $\Delta\sigma'_{av}$ | 5.81 kPa |
| Compression index, $C_c = 0.009(LL-10)$ | 0.252 |
| Primary consolidation settlement, $S_c$ | 16.9 mm |
| Same calculation with Boussinesq stresses | 20.2 mm |
Two other methods for the same settlement, and the data they need.
Method A — direct use of the laboratory $e$–$\log\sigma'$ curve, with the clay divided into sublayers. Instead of estimating $C_c$ from the liquid limit and treating the clay as a single layer, undisturbed samples are consolidated in an oedometer and the settlement is computed sublayer by sublayer as $S_c = \sum \Delta e_i H_i/(1+e_{0i})$, reading $\Delta e_i$ straight off the measured curve at each sublayer's own $\sigma'_0$ and $\Delta\sigma'$. This removes two approximations at once: the correlation for $C_c$, whose scatter is easily a factor of $\pm 30$ per cent, and the assumption that a single mid-layer stress represents a layer over which $\Delta\sigma'$ falls by a factor of three. Additional data required: undisturbed (Shelby tube or block) samples from at least three levels in the clay; a complete one-dimensional consolidation test on each, giving the $e$–$\log\sigma'$ curve, the preconsolidation pressure $\sigma'_c$ (Casagrande construction), the recompression index $C_r$ for the part of the increment below $\sigma'_c$, and the coefficient of consolidation $c_v$ so that the time–settlement curve can also be produced; plus measured $e_0$ and $\gamma$ for each sublayer.
Method B — the Skempton–Bjerrum method. The one-dimensional equation used above assumes zero lateral strain, which is true for a wide fill but not for a footing only 1.5 m wide over a 2.5 m clay layer: some of the applied stress is carried immediately by an undrained shear distortion, so the consolidation settlement is less than the oedometer prediction. Skempton and Bjerrum write $S_{c(SB)} = \mu\,S_{c(oed)}$, where the settlement ratio $\mu$ depends on the pore-pressure parameter $A$ and on the geometry ratio $H_c/B$; for a normally consolidated clay ($A \approx 0.5$ to $1.0$) under a square or circular footing $\mu$ typically lies between 0.6 and 1.0. The total settlement is then the sum of the immediate (undrained) settlement $S_i$, this corrected consolidation settlement, and secondary compression $S_s = C_{\alpha}H\log_{10}(t_2/t_1)/(1+e_p)$. Additional data required: the pore-pressure parameter $A$ at failure from CU triaxial tests with pore-pressure measurement on undisturbed samples; the undrained modulus $E_u$ (from the same triaxial tests or from a pressuremeter) and Poisson's ratio for the immediate settlement; the drainage geometry and $c_v$ for the rate; and the secondary compression index $C_{\alpha}$ from the long-term (24-hour-plus) portion of the oedometer curves.
A third possibility worth naming is the stress-path method of Lambe, in which the actual total-stress path followed by a representative element beneath the footing is reproduced in a triaxial cell and the strains are integrated over depth; it is the most realistic of the three but needs a large, specialised testing programme, including the initial $K_0$ state and the in-situ stress history.
Check — assumptions.