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18-Env-A3 Geotechnical and Hydrogeological Engineering · May 2015

Question 1 of 6: Compaction — Porosity, Saturation and Unit Weights

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

Notes on this paper

National Exams — May 2015 — 04-Env-A3 / Geotechnical & Hydrogeological Engineering. 3 hours duration; open book exam, any non-communicating calculator permitted. The first five questions as they appear in the answer book are marked (20 marks each, 100 marks total); all six are solved below for completeness.

Reference texts. Braja M. Das, Principles of Geotechnical Engineering (9th ed.) — weight–volume relations, USCS classification, seepage/flow nets, slope-stability and stress-distribution chapters; Craig & Knappett, Craig's Soil Mechanics (8th ed.) — flow-net construction and Taylor's stability-number method; Freeze & Cherry, Groundwater (1979) — Darcy's law and the Dupuit–Thiem equation for radial flow to a well.

Question 1: Compaction — Porosity, Saturation and Unit Weights (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
Mold volume$V$1.0 L = 0.001 m³
Compacted (moist) mass$M$1.850 kg
Moisture content$w$12%
Specific gravity of solids (assumed)$G_s$2.70

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

Approach. Compute the bulk density directly from the mold, strip out the moisture to get the dry unit weight, then use an assumed $G_s$ to back out the void ratio and complete the remaining phase relations.

  1. Part (c) — bulk (moist) density. The as-compacted density uses the whole mass over the mold volume: $$\rho=\frac{M}{V}=\frac{1.850}{0.001}=\boxed{1850\ \text{kg/m}^3}\quad\left(\gamma=\rho g=1850\times9.81/1000=18.15\ \text{kN/m}^3\right).$$
  2. Part (d) — dry unit weight. Strip the pore water using $w=M_w/M_s$: $$M_s=\frac{M}{1+w}=\frac{1.850}{1.12}=1.6518\ \text{kg},\qquad \rho_d=\frac{M_s}{V}=1651.8\ \text{kg/m}^3,$$ $$\gamma_d=\rho_d g=1651.8\times9.81/1000=\boxed{16.20\ \text{kN/m}^3}.$$
  3. Part (a) — void ratio and porosity. With $G_s=2.70$ assumed, inverting $\gamma_d=\dfrac{G_s}{1+e}\gamma_w$ gives $$e=\frac{G_s\,\gamma_w}{\gamma_d}-1=\frac{2.70\times9.81}{16.20}-1=0.6346,\qquad n=\frac{e}{1+e}=\frac{0.6346}{1.6346}=\boxed{38.8\%}.$$
  4. Part (b) — degree of saturation. $S=\dfrac{w\,G_s}{e}$: $$S=\frac{0.12\times2.70}{0.6346}=\boxed{51.1\%}.$$
  5. Part (e) — saturated unit weight. Flooding the same void ratio to $S=100\%$: $$\gamma_{sat}=\frac{G_s+e}{1+e}\,\gamma_w=\frac{2.70+0.6346}{1.6346}\times9.81=\boxed{20.01\ \text{kN/m}^3}.$$
Check: the exam supplies no specific gravity, so $G_s=2.70$ is assumed (typical for a mixed quartz/silicate mineral soil, per Das Table 3.1). A different reasonable $G_s$ (2.65–2.75) shifts every result by well under 2%.
QuantityValue
(a) Porosity, $n$38.8%
(b) Degree of saturation, $S$51.1%
(c) Bulk density, $\rho$ (unit weight $\gamma$)1850 kg/m³ (18.15 kN/m³)
(d) Dry unit weight, $\gamma_d$16.20 kN/m³
(e) Saturated unit weight, $\gamma_{sat}$20.01 kN/m³
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