Question 2 of 5: Open-pit wedge factor-of-safety derivation
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
Notes on this paper
National Exams, May 2016 — 04-Geol-A5, Rock Mechanics. Closed-book, 3-hour
exam; 5 questions of 20 marks each; candidates were instructed to answer only 4 of the 5 — all 5 are answered below as a complete study resource.
Reference texts for this subject:
Bieniawski, Z.T. (1989), Engineering Rock Mass Classifications, Wiley.
Hoek, E. (2007), Practical Rock Engineering, Rocscience (open-access course notes).
Brady, B.H.G. & Brown, E.T., Rock Mechanics for Underground Mining, 3rd ed.
Wyllie, D.C. & Mah, C.W., Rock Slope Engineering, 5th ed.
Barton, N., Lien, R. & Lunde, J. (1974), “Engineering Classification of Rock Masses for
the Design of Tunnel Support” (the NGI Q-system).
It does
not affect the solutions below, which are worked from the real printed question text on pages
3–5.
Given. A wedge bounded above by the horizontal ground surface, at the back by
the vertical pit face of height H, below/ahead by joint system A (dip ψ, cohesion c,
friction angle φ) which is the basal sliding surface, and laterally by two parallel joint-B
release planes spaced W apart, cohesionless (C = 0) and assumed to carry no net resisting force on
the block (their sole role is to isolate a finite-width wedge).
Left: cross-section of the sliding wedge (vertical pit face height H,
basal Joint A dipping at ψ). Right: front elevation of the pit face showing the
cohesionless Joint B release planes spaced W apart, which isolate one wedge block.
Find. An equation for the factor of safety, FoS, against sliding on Joint A, in
terms of the wedge/excavation geometry (H, ψ, W) and the shear-strength parameters (c, φ)
of Joint A.
Approach. Build the wedge as a triangular prism (cross-section area from the
geometry of H and ψ, length W into the pit face), resolve its self-weight into components
normal and parallel to the basal Joint-A plane, sum the resisting force (Joint A's cohesion plus
friction on the resolved normal force — Joint B contributes nothing, since it is cohesionless
and treated as a pure release surface) against the driving (down-dip) component of weight, and
simplify.
Wedge cross-sectional area. With no tension crack, the wedge cross-section is
the right triangle bounded by the vertical pit face (height H), the horizontal ground surface, and
Joint A running from the toe of the pit face up to the ground surface at dip ψ. The
horizontal run of Joint A is H/tanψ, so
$$A_{xsec}=\tfrac{1}{2}H\cdot\frac{H}{\tan\psi}=\frac{H^2}{2\tan\psi}$$
Wedge weight and Joint-A plane area. Extending the cross-section a distance W
into the pit face (the Joint-B spacing) gives the full 3D wedge:
$$W_{wedge}=\gamma\,A_{xsec}\,W=\frac{\gamma H^2 W}{2\tan\psi}$$
The length of Joint A within the cross-section is H/sinψ, so its area is
$$A_{JointA}=\frac{HW}{\sin\psi}$$
Resolve the weight on Joint A. The component of weight normal to Joint A drives
frictional resistance; the down-dip component is the driving force:
$$N=W_{wedge}\cos\psi,\qquad T=W_{wedge}\sin\psi$$
Resisting force. Joint A supplies both cohesion (over its full area) and
friction (on the resolved normal force); Joint B is cohesionless and, acting purely as a lateral
release surface, is taken to contribute no net resistance to sliding:
$$R=c\,A_{JointA}+N\tan\phi=\frac{cHW}{\sin\psi}+\frac{\gamma H^2W\cos\psi}{2\tan\psi}\tan\phi$$
Factor of safety and simplification.
$$FoS=\frac{R}{T}=\frac{\dfrac{cHW}{\sin\psi}+\dfrac{\gamma H^2W\cos\psi}{2\tan\psi}\tan\phi}{\dfrac{\gamma H^2W\sin\psi}{2\tan\psi}}$$
Every term carries a factor of W, which cancels between numerator and denominator — the wedge
width, and hence the Joint-B spacing, drops out of the factor of safety entirely. Simplifying the
remaining H, γ and trig terms gives the closed form
$$\boxed{FoS=\frac{2c+\gamma H\cos^2\psi\tan\phi}{\gamma H\sin\psi\cos\psi}=\frac{2c}{\gamma H\sin2\psi}+\frac{\tan\phi}{\tan\psi}}$$
Check: this is exactly the classical Hoek–Bray planar-failure factor of
safety for a slope of height H with a vertical face and no tension crack (dry, no water pressure) —
derived here from first principles for the stated wedge geometry, and cross-checked
(arbitrary illustrative ψ=40°, c=120 kPa, φ=35°, γ=26 kN/m³, H=30 m gives
FoS = 1.46 identically whether computed from the raw geometry with W = 15 m or W = 25 m, confirming
the algebraic cancellation).