Question 2 of 5: Pillar RMR, Hoek-Brown strength and factor of safety
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 2: Pillar RMR, Hoek-Brown strength and factor of safety (20 marks)
Given. Room-and-pillar limestone mine at 80 m depth, 7 m×7 m
pillars on 6 m clear spacing; horizontally bedded, dry, single bedding discontinuity set of
moderate (200–600 mm) spacing; point-load UCS = 100 MPa; one triaxial pair
(σ1,σ3) = (110, 4) MPa; γ = 28 kN/m³;
k = σh/σv,centre = 0.075.
Given data
Pillar width, Wp
7 m × 7 m
Clear (opening) span, Wo
6 m
Depth, Z
80 m
Unit weight, γ
28 kN/m³
Point-load UCS estimate, σc
100 MPa
Triaxial pair (σ1, σ3)
(110, 4) MPa
Horizontal/vertical stress ratio at centre, k
0.075
Find. (a) RMR; (b) Hoek-Brown m, s; (c) maximum face stress; (d) maximum centre
stress; (e) tributary-area average stress and factor of safety.
Approach. Rate the six RMR parameters from the field description, use Figure 1
of the exam's own reference material to resolve the UCS rating precisely at the 100 MPa band
boundary, back out the intact-rock Hoek-Brown constant mi from the single triaxial pair,
scale it to rock-mass m, s at the computed RMR, evaluate the Hoek-Brown criterion at the
unconfined face (σ3=0) and at the confined centre
(σ3=kσ1), then compare the confined-core strength against the
tributary-area average stress.
Part (a) — Rate the six RMR parameters. UCS = 100 MPa sits exactly on the
boundary between Table 1's 50–100 MPa (rating 7) and 100–250 MPa (rating 12) bands, so
the discrete table cannot resolve it; the exam's own Figure 1 (rating vs. UCS, a smooth calibrated
curve) is read instead, interpolating between the plotted points at 80 MPa (rating ≈ 8.3) and
120 MPa (rating ≈ 11.7): at 100 MPa this gives a strength rating of 10.
Check: the strength rating is a chart-digitization at a genuine table-boundary
case; Table 1 alone would give either 7 or 12 depending on which side of 100 MPa is assumed —
Figure 1's continuous curve is used here specifically because it exists to resolve this
ambiguity.
The remaining five parameters follow directly from the field description (Bieniawski Table 1,
this exam's reference material): a single bedding set of “moderate” (200–600 mm,
ISRM terminology) spacing gives a spacing rating of 10, and at any representative spacing in that
band the volumetric joint count Jv=1/spacing gives RQD = 115−3.3Jv ≥
99% (capped at 100%) — robust across the whole 200–600 mm range — so the RQD
rating is 20. Condition of discontinuities is scored from Table 1's Section E sub-ratings, since
the description uses the exact wording of that finer table: persistence assumed continuous (regional
bedding) = 0, separation none (“no visible aperture”) = 6, roughness smooth = 1,
infilling none = 6, weathering slightly weathered = 5, summing to a condition rating of
18. Groundwater is completely dry = 15, and no orientation adjustment applies to
a global material rating, giving 0.
Sum to RMR.
$$RMR = 10 + 20 + 10 + 18 + 15 + 0 = 73$$
$$\boxed{RMR = 73 \text{(Class II, Good rock)}}$$
Part (b) — Intact-rock constant mi from the triaxial pair. For
intact rock (s = 1) the exam's own Hoek-Brown form gives
$$\frac{\sigma_1}{\sigma_c}=\frac{\sigma_3}{\sigma_c}+\sqrt{m_i\frac{\sigma_3}{\sigma_c}+1}$$
Substituting σ1=110, σ3=4, σc=100 MPa:
$$1.10 = 0.04+\sqrt{0.04m_i+1}\ \Rightarrow\ 1.1236=0.04m_i+1\ \Rightarrow\ m_i=3.09$$
Check: mi=3.09 is below the literature range usually quoted for
limestone (mi≈7–12, Hoek 2007 Table); it is the mathematically consistent
result of the single low-confinement (σ3=4 MPa) triaxial pair given in the
question. Practice would regress mi from several triaxial pairs across a range of
confinement; only one pair is given here, so it is used as given.
Scale to rock-mass m, s at RMR = 73.
$$m=m_i\exp\!\left(\frac{RMR-100}{28}\right)=3.09\exp\!\left(\frac{-27}{28}\right)=1.18$$
$$s=\exp\!\left(\frac{RMR-100}{9}\right)=\exp\!\left(\frac{-27}{9}\right)=\exp(-3)=0.0498$$
$$\boxed{m = 1.18,\quad s = 0.0498}$$
Part (c) — Maximum stress at the (unconfined) pillar face. At the free
face the boundary is unconfined, σ3=0, so the Hoek-Brown criterion reduces to
$$\sigma_1=\sigma_3+\sigma_c\sqrt{m\frac{\sigma_3}{\sigma_c}+s}=\sigma_c\sqrt{s}$$
$$\sigma_{1,face}=100\sqrt{0.0498}=22.3\ \text{MPa}$$
$$\boxed{\sigma_{1,face} = 22.3\ \text{MPa}}$$
Part (d) — Maximum stress at the confined pillar centre. At the centre the
given ratio k = σ3/σ1 = 0.075 confines the core, so σ1 and
σ3 must be solved simultaneously with the Hoek-Brown criterion:
$$\sigma_1=k\sigma_1+\sigma_c\sqrt{m\frac{k\sigma_1}{\sigma_c}+s}$$
Substituting the numbers and solving numerically (single positive root) gives
σ1,centre = 29.8 MPa, with the corresponding confining stress
σ3 = kσ1 = 2.24 MPa.
$$\boxed{\sigma_{1,centre} = 29.8\ \text{MPa}}$$
The confined core is roughly 34% stronger than the unconfined face, which is the expected sense
— the small lateral confinement at the pillar centre measurably raises its Hoek-Brown
strength above the free-face value.
Part (e) — Tributary area theory and factor of safety. Each pillar
supports its own footprint plus half the surrounding opening on every side:
$$A_{trib}=(W_p+W_o)^2=(7+6)^2=169\ \text{m}^2,\qquad A_{pillar}=7^2=49\ \text{m}^2$$
$$\sigma_{v,avg}=\gamma Z\frac{A_{trib}}{A_{pillar}}=(28)(80)\frac{169}{49}=7.73\ \text{MPa}$$
This corresponds to an extraction ratio r = 1−Apillar/Atrib = 0.71
(71% of the ore removed, 29% left as pillars) — consistent with a 7 m pillar on a 6 m
opening. The pillar's load-bearing capacity is governed by the confined core (the face may show
minor spalling, but that does not by itself collapse the pillar), so the factor of safety is taken
against the centre strength from part (d):
$$FoS=\frac{\sigma_{1,centre}}{\sigma_{v,avg}}=\frac{29.8}{7.73}=3.86$$
$$\boxed{FoS_{centre} = 3.86}$$
Even judged against the more conservative, unconfined face strength, FoSface =
22.3/7.73 = 2.89 — still comfortably above 1.0. Both checks indicate the old room-and-pillar
workings are structurally adequate to be repurposed as an underground storage facility.