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16-Civ-B3 Geotechnical Design · May 2016

Question 4 of 9: Field methods for soil strength, and their limitations (7 marks)

Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)

Notes on this paper

Paper format. Professional Engineers Ontario / Engineers Canada National Examinations, May 2016 — 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 requires the candidate to identify the source of every design chart used and of every value assumed where the paper gives none. They are named at the point of use and collected here:

  • Strain-influence diagram and the C₁, C₂ correction factors (Q6) — Schmertmann, Hartman and Brown (1978), as tabulated in Das, Principles of Foundation Engineering, 9th ed., Section 5.6.
  • Rankine active coefficient for an inclined backfill (Q7) — Das, Principles of Geotechnical Engineering, 9th ed., Eq. (13.35).
  • Bearing-capacity factors N₢, Nᵤ, Nγ and the depth and load- inclination factors (Q7) — Vesic / Meyerhof as tabulated in Das, Principles of Foundation Engineering, 9th ed., Tables 3.3 and 3.4, applied to a retaining-wall base in Section 8.6.
  • Meyerhof bearing-capacity factor Nᵤ* for a driven pile point and the limiting point resistance (Q8) — Das, 9th ed., Section 11.9 and its interpolated Nᵤ* table; Nᵤ* = 143 at φ′ = 35°.
  • Adhesion factor α against cu/p₀ (Q8) — Das, 9th ed., Table 11.6 (after Terzaghi, Peck and Mesri); α = 0.68 at cu/p₀ = 0.5.
  • Earth-pressure coefficient K and interface friction angle δ′ for a driven high-displacement pile (Q8) — Das, 9th ed., Section 11.11: K ≈ 1.4K₀ and δ′ ≈ 0.8φ′ are assumed, and the critical-depth rule L′ = 15D is Das Eq. (11.42).
  • Unit weight of water γᵣ = 9.81 kN/m³ and g = 9.81 m/s² throughout; atmospheric pressure p₀ = 100 kPa.

Section A — discussion questions (7 marks each)

Question 4 — Field methods for soil strength, and their limitations (7 marks)

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.

Methods available in the field. The in-situ tests in ordinary Canadian practice, in roughly increasing order of sophistication, are: the standard penetration test (SPT) with split-spoon sampling; the cone penetration test and its piezocone variant (CPT / CPTu), optionally with a seismic module; the field vane shear test (VST); the flat dilatometer test (DMT); the pressuremeter test, either pre-bored (Menard) or self-boring; the plate load test and the screw plate test; the borehole shear test; the Becker penetration test for gravels and tills; and geophysical methods (seismic cross-hole, down-hole and surface-wave surveys) that return the small-strain shear modulus $G_{\max} = \rho V_s^{2}$ rather than a strength. To these should be added the quasi-field index tools used on recovered samples at the borehole — the pocket penetrometer and the torvane — which are useful for logging but are not design tests.

The rapid method for a dense sand: the cone penetration test. The CPT pushes a 10 cm2 cone at 20 mm/s and logs tip resistance $q_c$ and sleeve friction $f_s$ continuously, so a 20 m profile is obtained in well under an hour and the friction angle follows from established correlations such as $\phi' = \tan^{-1}\!\left[0.1 + 0.38\log\left(q_c/\sigma'_{v0}\right)\right]$ (Robertson and Campanella — the same source as the profile used in Question 6). Where the sand is gravelly or contains cobbles the SPT is the practical alternative, with $\phi'$ taken from $N_{60}$ corrected for overburden to $\left(N_1\right)_{60}$.

The rapid method for a soft clay: the field vane test. The vane is pushed into undisturbed clay below the borehole and rotated at about 6° per minute; the peak torque gives the undrained strength directly, $c_u = \dfrac{T}{\pi d^{2}\left(h/2 + d/6\right)}$ for a rectangular vane, and rotating the vane rapidly through ten turns and re-testing gives the remoulded strength and hence the sensitivity in the same operation. CPTu is the natural companion, giving a continuous profile through $c_u = \left(q_t - \sigma_{v0}\right)/N_{kt}$.

Limitations of each.

The practical conclusion is that no single test is sufficient. Canadian practice, and the CFEM, recommend a combination: continuous CPTu profiling to define the stratigraphy and the trend of strength with depth, calibrated at intervals by boreholes with SPT and sampling in coarse soils and by field vane tests in soft clays, with laboratory triaxial and oedometer testing on the best samples to anchor the correlations.