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18-Env-A3 Geotechnical and Hydrogeological Engineering · May 2014

Question 1 of 6: Compaction — Weight–Volume Relations

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

Notes on this paper

National Exams — May 2014 — 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, consolidation and slope-stability chapters; Craig & Knappett, Craig's Soil Mechanics (8th ed.) — cross-reference for consolidation theory 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 — Weight–Volume Relations (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$1.820 kg
Moisture content$w$7%
Specific gravity of solids$G_s$2.6

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. Split the moist mass into dry-solids and water masses using $w=M_w/M_s$, convert the dry mass to a solids volume via $G_s$, then read every weight–volume ratio off the resulting phase diagram.

  1. Part (a)/(b) — split the compacted mass and find the phase volumes. With $w=M_w/M_s$, $$M_s=\frac{M}{1+w}=\frac{1.820}{1.07}=1.70094\ \text{kg}, \qquad M_w=M-M_s=0.11907\ \text{kg}.$$ The solids volume follows from $G_s=M_s/(\rho_w V_s)$: $$V_s=\frac{M_s}{G_s\,\rho_w}=\frac{1.70094}{2.6\times1000}=6.5421\times10^{-4}\ \text{m}^3=654.2\ \text{cm}^3.$$ The void volume is the remainder of the 1000 cm³ mold: $V_v=V-V_s=1000-654.2=345.8\ \text{cm}^3$, so $$n=\frac{V_v}{V}=\frac{345.8}{1000}=\boxed{34.6\%}.$$
  2. Degree of saturation. The water occupies $V_w=M_w/\rho_w=119.1\ \text{cm}^3$ (since $\rho_w=1\ \text{g/cm}^3$), and $$S=\frac{V_w}{V_v}=\frac{119.1}{345.8}=\boxed{34.4\%}.$$
  3. Part (c) — bulk density. The as-compacted (moist) density uses the total mass over the mold volume: $$\rho=\frac{M}{V}=\frac{1.820\ \text{kg}}{0.001\ \text{m}^3}=\boxed{1820\ \text{kg/m}^3}.$$
  4. Part (d) — dry unit weight. The dry density is $\rho_d=M_s/V=1700.9\ \text{kg/m}^3$, so $$\gamma_d=\rho_d\,g=1700.9\times9.81/1000=\boxed{16.69\ \text{kN/m}^3}.$$
  5. Part (e) — saturated unit weight. Compaction does not change the void ratio $e=V_v/V_s=345.8/654.2=0.5286$, so filling every void with water ($S=100\%$) gives $$\gamma_{sat}=\frac{G_s+e}{1+e}\,\gamma_w=\frac{2.6+0.5286}{1.5286}\times9.81=\boxed{20.08\ \text{kN/m}^3}.$$
Check: part (e) assumes the SAME void ratio the mold was compacted to ($e=0.5286$) is simply flooded to full saturation — i.e. it is not a re-compaction at a different density, which is the standard interpretation of "saturated unit weight of this soil."
QuantityValue
(a) Porosity, $n$34.6%
(b) Degree of saturation, $S$34.4%
(c) Bulk density, $\rho$1820 kg/m³
(d) Dry unit weight, $\gamma_d$16.69 kN/m³
(e) Saturated unit weight, $\gamma_{sat}$20.08 kN/m³
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