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.
B. M. Das, Principles of Foundation Engineering, 9th ed. — subsurface
exploration (Ch. 2), bearing capacity of shallow foundations (Ch. 3), settlement of
shallow foundations including Schmertmann's method (Ch. 5), retaining walls (Ch. 8),
pile foundations (Ch. 11).
B. M. Das, Principles of Geotechnical Engineering, 9th ed. — shear
strength (Ch. 12), lateral earth pressure (Ch. 13), slope stability including the
planar-surface analysis (Ch. 15).
Canadian Geotechnical Society, Canadian Foundation Engineering Manual
(CFEM), 4th ed. — the governing Canadian practice document for site investigation,
in-situ testing, bearing resistance, deep foundations and earth-retaining structures.
R. F. Craig, Craig's Soil Mechanics, 9th ed. — effective stress,
undrained versus drained behaviour, earth pressure and slope stability.
D. P. Coduto, Foundation Design: Principles and Practices, 3rd ed. —
CPT correlations and settlement of shallow foundations on sand.
M. J. Tomlinson & J. Woodward, Pile Design and Construction Practice,
6th ed. — shaft adhesion in clay and driven displacement piles in sand.
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)
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.
CPT / CPTu. No sample is recovered, so the soil must be classified from the
friction ratio and pore-pressure response rather than seen; the strength values are
correlations, not measurements, and the cone factor $N_{kt}$ ranges from about 10 to 20 so
the derived $c_u$ carries a real uncertainty; a heavy reaction mass (typically a 15 to
20 tonne truck or anchored rig) is needed and access can be impossible; the cone refuses in
dense gravel, cobbles or till and can be damaged; readings must be corrected for unequal
end area to $q_t$, and in a very dense sand the tip load may exceed the rating of the
cone.
SPT. The single most variable test in geotechnics: the energy actually
delivered to the rods depends on the hammer, and raw N must be converted to $N_{60}$;
results are affected by rod length, borehole diameter, sampler liners, and by disturbance
or base heave in the borehole; gravel or cobbles jamming the shoe give spuriously high
blow counts; in soft clay N is near zero and carries no useful information; the sample is
disturbed, so it serves only for classification; and every strength interpretation is
empirical, with no modulus obtained at all.
Field vane. Applicable only to soft to firm clays — it cannot be pushed
into stiff clay, sand or till; it measures strength on a vertical cylindrical surface, so
it reflects anisotropy in an unrepresentative way; it systematically over-estimates
the strength mobilised in a field embankment failure, which is why Bjerrum's correction
factor $\mu\!\left(\text{PI}\right)$ (falling from 1.0 at low plasticity to about 0.6 at
PI = 60) must be applied; sand or silt partings and fissures in the clay give erratically
high torques; the result is rate dependent; and it gives only the undrained strength, never
$c'$, $\phi'$ or any stiffness.
Pressuremeter and dilatometer (mentioned for completeness). Both give strength
and stiffness in one test, but the pre-bored pressuremeter is highly sensitive to the
quality of the pocket, the self-boring version is expensive and slow, and both require
skilled operators and careful interpretation.
Plate load test. Direct and easy to interpret, but it stresses only about
twice the plate width of soil, so it misses deeper compressible layers entirely, and the
scale effect between a 300 mm plate and a real footing must be corrected for; it is slow
and costly and is normally reserved for confirming a design rather than making one.
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.