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18-Geol-A5 Rock Mechanics · Undated paper

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:

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)

Question text not reproduced: the examination questions are © Engineers and Geoscientists BC. Open the official past paper (linked at the top of this page) to read the question, then follow the worked solution below.

Given.

Two rock-mass classification scenarios
Parameter(a) Granite(b) Sandstone
Joint sets3, spacing 0.24 m each2 sets + random fractures
RQDnot given — from $J_v$70% (given)
Spacing0.24 m (240 mm)0.11 m (110 mm)
Joint conditionsmooth, weathered, occasional stainsslightly rough, slightly weathered, staining, cleaned, aperture <1 mm
Groundwaterwet, not drippingwater table 10 m below surface; tunnel at 80 m (submerged)
UCS160 MPa85 MPa
Depth150 m, no abnormal stress80 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 $Q=\tfrac{RQD}{J_n}\times\tfrac{J_r}{J_a}\times\tfrac{J_w}{SRF}$.

  1. (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).
  2. (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). $$RMR=12+13+10+20+7-5=\boxed{57}\ \Rightarrow\ \text{Class III (Fair rock)}$$
  3. (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.
  4. (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 ($-5$). $$RMR=7+13+8+25+7-5=\boxed{55}\ \Rightarrow\ \text{Class III (Fair rock)}$$
  5. (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.
ScenarioRQDRMRClassQQ class
(a) Granite73.75%57III – Fair4.10C – Fair
(b) Sandstone70% (given)55III – Fair17.3B – Good