Question 4 of 5: Plane failure with a water-filled tension crack
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
Notes on this paper
National Exams, December 2015 — 04-Geol-A5, Rock Mechanics. Open-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).
Question 4: Plane failure with a water-filled tension crack (20 marks)
Given. Slope height H = 30 m; face AB at 60° to horizontal; horizontal crest
distance BC = b = 8.66 m; fracture plane AD dips 30°; c = 20 kPa, φ = 30°;
γrock = 25 kN/m³, γwater = 10 kN/m³.
Find. (a) general FoS(zw) equation; (b) FoS with the tension crack
dry; (c) FoS with the tension crack full of water, and whether it explains the observed winter
failure.
Approach. Fix the block geometry (A, B, C, D) from the given angles and
dimensions, express the block weight and the two water forces (uplift on AD, thrust on CD) in terms
of the unknown crack water depth zw, then assemble the limit-equilibrium factor of
safety as resisting force over driving force along the sliding plane.
Part (a) — Fix the block geometry. Taking A as the origin with the face
rising at 60°: B = (H/tan60°, H) = (17.32, 30) m. The crest surface runs horizontally a
further b = 8.66 m to C = (25.98, 30) m. The tension crack is vertical, so D lies on plane AD
directly below C; solving the plane AD (dip 30° from A) for the same x-coordinate as C gives
D = (25.98, 15.00) m. This gives a sliding-plane length and a tension-crack depth of
$$L_{AD}=|AD|=30.0\ \text{m},\qquad z=|CD|=H-D_y=15.0\ \text{m}$$
i.e. the tension crack reaches exactly to mid-height of the slope — a useful internal check on
the figure's stated dimensions. Simplifying assumptions: the slide is a rigid 2-D
block on a planar surface of unit thickness (plane-strain, per metre of slope length); the tension
crack is vertical and dry above any water level in it; when water is present it fills the crack to
depth zw and seeps along AD, dissipating linearly from a peak of
γwzw at D to zero at the toe A (a standard triangular pressure
distribution); no seismic or external load is applied; shear strength on AD is Mohr-Coulomb
(c, φ) with no scale effect.
Weight of the block. The cross-sectional area of quadrilateral ABCD (shoelace
formula on A, B, C, D) is 324.8 m² per metre of slope length, so
$$W=\gamma_{rock}\times\text{Area}=25\times324.8=8119\ \text{kN/m}$$
Water forces as a function of zw. The triangular uplift pressure
along AD (peak γwzw at D, zero at A) resultant is
$$U=\tfrac12\gamma_w z_w L_{AD}$$
and the triangular horizontal thrust on the vertical crack face CD (peak
γwzw at D, zero at the water surface) resultant is
$$V=\tfrac12\gamma_w z_w^2$$
Part (a) — Assemble the factor of safety. Resolving forces parallel and
normal to plane AD (dip ψp=30°), the driving component is the down-dip weight
component plus the down-dip component of V; the resisting component is cohesion over the full
plane area plus friction on the effective (uplift-reduced) normal force:
$$\boxed{FoS(z_w)=\frac{cL_{AD}+\big[W\cos\psi_p-U-V\sin\psi_p\big]\tan\phi}{W\sin\psi_p+V\cos\psi_p}}$$
with U and V from the previous step, both functions of the single unknown zw.
Part (b) — Dry conditions (mid-summer). With zw=0, U=V=0 and
the equation collapses to the simple dry form:
$$FoS_{dry}=\frac{cL_{AD}+W\cos\psi_p\tan\phi}{W\sin\psi_p}=\frac{(20)(30)+8119\cos30^\circ\tan30^\circ}{8119\sin30^\circ}$$
$$\boxed{FoS_{dry} = 1.15}$$
The slope was therefore stable (FoS > 1) when it was excavated in dry mid-summer conditions,
consistent with no failure being reported at that time.
Part (c) — Saturated tension crack (winter). Heavy winter rain is taken as
the critical, worst-case condition of the crack filling completely to the surface,
zw = z = 15.0 m (the tension-crack depth found in step 1), giving
U = ½(10)(15.0)(30.0) = 2250 kN/m and V = ½(10)(15.0)² = 1125 kN/m. Substituting
into the part (a) equation:
$$FoS_{wet}=\frac{(20)(30)+\big[8119\cos30^\circ-2250-1125\sin30^\circ\big]\tan30^\circ}{8119\sin30^\circ+1125\cos30^\circ}$$
$$\boxed{FoS_{wet} = 0.60}$$
Since FoSwet = 0.60 < 1.0, the computed factor of safety does predict
failure under a saturated tension crack — the uplift force U and crack thrust V together remove
enough of the plane's normal confinement and add enough down-dip driving force that the same
geometry and material that was stable dry (FoS 1.15) becomes unstable when the tension crack fills
with water (FoS 0.60). This is fully consistent with the slope standing through dry mid-summer and
then failing after the winter rain saturated the crack.
Final results — Question 4
Sliding-plane length LAD
30.0 m
Tension-crack depth z
15.0 m
Block weight W
8119 kN per m of slope width
General FoS(zw)
see boxed equation, step 4
FoS, dry (part b)
1.15 — stable
FoS, crack saturated (part c)
0.60 — predicts failure, matches the observed
winter failure