Question 3 of 5: RMR and Q classification for two tunnel scenarios
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
Notes on this paper
National Exams — 18-Geol-A5, Rock Mechanics. Closed-book, 3-hour exam; 5 questions
of 20 marks each (80 marks total); candidates were instructed to answer only 4 of the 5 — all 5 are answered below. Every page footer of the paper reads “May 2019”.
Reference texts:
Bieniawski, Z.T. (1989), Engineering Rock Mass Classifications, Wiley.
Barton, N., Lien, R. & Lunde, J. (1974), “Engineering Classification of Rock Masses for the
Design of Tunnel Support” (the NGI Q-system).
Brady, B.H.G. & Brown, E.T., Rock Mechanics for Underground Mining, 3rd ed. (Kirsch
solution, pillar/tributary-area interaction).
Hoek, E. (2007), Practical Rock Engineering, Rocscience (open-access course notes; EDZ,
Mohr–Coulomb design).
Wyllie, D.C. & Mah, C.W., Rock Slope Engineering, 5th ed. (groundwater/vibration effects on
slope stability).
page-1 NOTES
items (1–8), the Additional-Reference-Material section's own numbered Table/Figure captions (e.g. “1. Strength of intact rock material…”, “5. Groundwater…”, “Figure
6…”), and stray numbered lines bled from inside a question's own paragraph. It does not affect the solutions
below, which are worked from the real printed question text (verified against the printed paper pages).
A few words of Question 5 are assumed from context. Page 8's thick-wall-cylinder formula prints “$P_r$” where the algebra requires a tangential stress; the standard thick-wall tangential-stress form is used below. The RMR discontinuity-spacing rating chart on page 12 is not used, because Table 1 (page 9) gives the same information in exact numeric form.
Question 3: RMR and Q classification for two tunnel scenarios (20 marks)
slightly rough, slightly weathered, staining, cleaned, aperture <1 mm
Groundwater
wet, not dripping
water table 10 m below surface; tunnel at 80 m (submerged)
UCS
160 MPa
85 MPa
Depth
150 m, no abnormal stress
80 m
Find. RMR (Bieniawski 1989) and Q (Barton NGI) for each rock mass.
Approach. For (a), where RQD is not directly given, estimate it from the volumetric
joint count $RQD=115-3.3J_v$ using the stated joint-set spacing; for (b), RQD is given directly. Rate each
of RMR's five parameters against Table 1 (page 9 of the exam), apply the tunnel-orientation
adjustment, and read the rock class off Table 1C. For Q, select $J_n$, $J_r$, $J_a$, $J_w$ and SRF from
the Barton descriptors matching the stated joint-set count, surface condition and groundwater/stress
setting, then combine as $Q=\tfrac{RQD}{J_n}\times\tfrac{J_r}{J_a}\times\tfrac{J_w}{SRF}$.
(a) Granite — RQD from volumetric joint count. Three joint sets each spaced
0.24 m give $J_v=3/0.24=12.5$ joints/m, so
$$RQD=115-3.3(12.5)=\boxed{73.75\%}$$
which falls in Table 1's 50–75% bracket (rating 13).
(a) Granite — RMR. UCS 160 MPa → strength rating 12 (100–250 MPa
band); spacing 240 mm → rating 10 (200–600 mm band); condition (“smooth…
weathered with occasional stains”, between the slightly-rough/highly-weathered and slickensided
brackets) → rating 20 (engineering judgement, flagged below); groundwater “wet, not dripping”
→ rating 7; orientation unstated → assume Fair ($-5$, per Table 1B).
$$RMR=12+13+10+20+7-5=\boxed{57}\ \Rightarrow\ \text{Class III (Fair rock)}$$
(a) Granite — Q system. Three joint sets → $J_n=9$; smooth surfaces →
$J_r=1.0$; slightly altered/stained, non-softening → $J_a=2.0$; wet not dripping → $J_w=1.0$; no
abnormal stress at moderate depth → $SRF=1.0$.
$$Q=\frac{73.75}{9}\times\frac{1.0}{2.0}\times\frac{1.0}{1.0}=\boxed{4.10}$$
Per the exam's own Rock Classes table (page 14), $Q=4$–10 is class C (“Fair”) —
consistent with the RMR Class III result.
(b) Sandstone — RMR. UCS 85 MPa → rating 7 (50–100 MPa band);
RQD 70% → rating 13; spacing 110 mm → rating 8 (60–200 mm band); condition
(“slightly rough…slightly weathered…separation <1 mm”) matches Table 1's
own wording exactly → rating 25; groundwater (tunnel 70 m below the water table, no inflow rate
stated) assumed “Wet” → rating 7 (flagged below); orientation unstated → Fair
($-5$).
$$RMR=7+13+8+25+7-5=\boxed{55}\ \Rightarrow\ \text{Class III (Fair rock)}$$
(b) Sandstone — Q system. Two joint sets plus random → $J_n=4$; slightly rough
→ $J_r=1.5$; unaltered walls, staining only, generally cleaned → $J_a=1.0$; submerged 70 m
below the water table, no inflow-rate given → medium inflow/pressure assumed, $J_w=0.66$; SRF=1.0.
$$Q=\frac{70}{4}\times\frac{1.5}{1.0}\times\frac{0.66}{1.0}=\boxed{17.3}$$
This lands in the $Q=10$–40 (“Good”) band — one notch better than the RMR Class III
result, which is an expected feature of comparing two independently-calibrated empirical systems on
judgement-heavy inputs (condition/water descriptors), not a computational inconsistency.
Check: several inputs are engineering judgement calls the source text does not pin
down exactly — (a)'s joint-condition rating (smooth+weathered sits between two Table 1 brackets),
both scenarios' orientation adjustment (no strike/dip vs. tunnel-axis data given, so “Fair” is
assumed), and (b)'s groundwater $J_w$ (the water table depth is given but not an inflow rate). A site
investigation would replace each with a measured value.