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.
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.
Part (a) — bulk unit weight. The whole moist sample over its total volume:
$$\rho=\frac{M_t}{V}=\frac{1.8}{0.001}=1800\ \text{kg/m}^3,\qquad \gamma=\rho g=1800\times9.81/1000=\boxed{17.66\ \text{kN/m}^3}.$$
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).
Part (b) — dry density. $\rho_d=\dfrac{M_s}{V}=\dfrac{1.7}{0.001}=\boxed{1700\ \text{kg/m}^3}$ ($\gamma_d=1700\times9.81/1000=16.68\ \text{kN/m}^3$).
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: $n=e/(1+e)=0.4706/1.4706=0.320$✓).
Part (c) — degree of saturation. $S=\dfrac{V_w}{V_v}=\dfrac{100}{320}=\boxed{31.25\%}.$
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.