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18-Env-A3 Geotechnical and Hydrogeological Engineering · May 2017

Question 1 of 6: Soil Phase Relationships

Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)

Notes on this paper

National Exams — May 2017 — 04-Env-A3 / Geotechnical & Hydrogeological Engineering. 3 hours duration; open book exam, any non-communicating calculator permitted. FIVE (5) questions constitute a complete exam paper (the first five as they appear in the answer book are marked, 20 marks each, 100 marks total); all six printed questions are solved below for completeness.

Reference texts. Braja M. Das, Principles of Geotechnical Engineering (9th ed.) — weight–volume relations, seepage/flow nets, grain-size analysis, consolidation and slope-stability chapters; Craig & Knappett, Craig's Soil Mechanics (8th ed.) — cross-reference for flow-net theory and the Method of Fragments; Freeze & Cherry, Groundwater (1979) — Darcy's law and the Dupuit–Thiem equation for radial flow to a well.

Question 1: Soil Phase Relationships (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.

Given data
QuantitySymbolValue
Total (moist) mass$M_t$1.8 kg
Total volume$V$1.0 L = 0.001 m³
Oven-dry mass$M_s$1.7 kg
Specific gravity of solids$G_s$2.5

Find. (a) bulk unit weight $\gamma$; (b) dry density $\rho_d$; (c) degree of saturation $S$; (d) saturated unit weight $\gamma_{sat}$; (e) porosity $n$.

Approach. Use the measured mass and volume to get the water mass directly, find the solids and void volumes from $G_s$, and combine into every requested phase ratio.

  1. Part (a) — bulk unit weight. The whole moist sample over its total volume: $$\rho=\frac{M_t}{V}=\frac{1.8}{0.001}=1800\ \text{kg/m}^3,\qquad \gamma=\rho g=1800\times9.81/1000=\boxed{17.66\ \text{kN/m}^3}.$$
  2. Volumes of solids, water and voids. $V_s=\dfrac{M_s}{G_s\rho_w}=\dfrac{1.7}{2.5\times1000}=6.80\times10^{-4}\ \text{m}^3$ (680 cm³); mass of water $M_w=M_t-M_s=0.1$ kg, so $V_w=1.00\times10^{-4}\ \text{m}^3$ (100 cm³); void volume $V_v=V-V_s=3.20\times10^{-4}\ \text{m}^3$ (320 cm³).
  3. Part (b) — dry density. $\rho_d=\dfrac{M_s}{V}=\dfrac{1.7}{0.001}=\boxed{1700\ \text{kg/m}^3}$ ($\gamma_d=1700\times9.81/1000=16.68\ \text{kN/m}^3$).
  4. Part (e) — porosity and void ratio. $n=\dfrac{V_v}{V}=\dfrac{320}{1000}=\boxed{32.0\%}$, and equivalently $e=\dfrac{V_v}{V_s}=\dfrac{320}{680}=0.4706$ (check: $n=e/(1+e)=0.4706/1.4706=0.320$✓).
  5. Part (c) — degree of saturation. $S=\dfrac{V_w}{V_v}=\dfrac{100}{320}=\boxed{31.25\%}.$
  6. Part (d) — saturated unit weight. Flood the same void space to $S=100\%$: total saturated mass $M_{sat}=M_s+V_v\rho_w=1.7+0.32=2.02$ kg, so $$\gamma_{sat}=\frac{M_{sat}}{V}g=\frac{2.02}{0.001}\times9.81/1000=\boxed{19.82\ \text{kN/m}^3}.$$
Check: all five results cross-check against the standard $G_s$/$e$ relations ($\gamma_d=G_s\gamma_w/(1+e)$, $\gamma_{sat}=(G_s+e)\gamma_w/(1+e)$, $\gamma=(1+w)G_s\gamma_w/(1+e)$ with $w=M_w/M_s=5.88\%$) to within rounding, confirming internal consistency of the phase diagram.
QuantityValue
(a) Bulk unit weight, $\gamma$17.66 kN/m³
(b) Dry density, $\rho_d$1700 kg/m³ (16.68 kN/m³)
(c) Degree of saturation, $S$31.25%
(d) Saturated unit weight, $\gamma_{sat}$19.82 kN/m³
(e) Porosity, $n$32.0% ($e=0.4706$)
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