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.
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.
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
$$n=\frac{V_v}{V}=\frac{345.8}{1000}=\boxed{34.6\%}.$$
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
$$S=\frac{V_w}{V_v}=\frac{119.1}{345.8}=\boxed{34.4\%}.$$
Part (c) — bulk density. The as-compacted (moist) density uses the total mass over the mold volume:
$$\rho=\frac{M}{V}=\frac{1.820\ \text{kg}}{0.001\ \text{m}^3}=\boxed{1820\ \text{kg/m}^3}.$$
Part (d) — dry unit weight. The dry density is $\rho_d=M_s/V=1700.9\ \text{kg/m}^3$, so
$$\gamma_d=\rho_d\,g=1700.9\times9.81/1000=\boxed{16.69\ \text{kN/m}^3}.$$
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."