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)
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.
Part (c) — bulk (moist) density. The as-compacted density uses the whole mass over the mold volume:
$$\rho=\frac{M}{V}=\frac{1.850}{0.001}=\boxed{1850\ \text{kg/m}^3}\quad\left(\gamma=\rho g=1850\times9.81/1000=18.15\ \text{kN/m}^3\right).$$
Part (d) — dry unit weight. Strip the pore water using $w=M_w/M_s$:
$$M_s=\frac{M}{1+w}=\frac{1.850}{1.12}=1.6518\ \text{kg},\qquad \rho_d=\frac{M_s}{V}=1651.8\ \text{kg/m}^3,$$
$$\gamma_d=\rho_d g=1651.8\times9.81/1000=\boxed{16.20\ \text{kN/m}^3}.$$
Part (a) — void ratio and porosity. With $G_s=2.70$ assumed, inverting $\gamma_d=\dfrac{G_s}{1+e}\gamma_w$ gives
$$e=\frac{G_s\,\gamma_w}{\gamma_d}-1=\frac{2.70\times9.81}{16.20}-1=0.6346,\qquad n=\frac{e}{1+e}=\frac{0.6346}{1.6346}=\boxed{38.8\%}.$$
Part (b) — degree of saturation. $S=\dfrac{w\,G_s}{e}$:
$$S=\frac{0.12\times2.70}{0.6346}=\boxed{51.1\%}.$$
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%.