18-Env-A3 Geotechnical and Hydrogeological Engineering · May 2016
Question 1 of 6: Weight–Volume Relations of a Soil
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
Notes on this paper
National Exams — May 2016 — 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, USCS classification, seepage/flow nets, consolidation and bearing-capacity chapters; Craig & Knappett, Craig's Soil Mechanics (8th ed.) — cross-reference for seepage and flow-net theory; Freeze & Cherry, Groundwater (1979) — Darcy's law, the Dupuit–Thiem equation for an unconfined well, and wellhead time-of-travel capture zones.
Question 1: Weight–Volume Relations of a Soil (20 marks)
Find. (a) void ratio $e$; (b) porosity $n$; (c) degree of saturation $S$; (d) moisture content $w$; (e) buoyant unit weight $\gamma_b$.
Approach. Back out the void ratio from $\gamma_d=G_s\gamma_w/(1+e)$, then read porosity and moisture content directly off it, use $wG_s=Se$ for saturation, and finally compute the saturated unit weight at the SAME void ratio to get the buoyant (submerged) unit weight.
Part (a) — void ratio from the dry unit weight. Since $\gamma_d=\dfrac{G_s\gamma_w}{1+e}$,
$$e=\frac{G_s\gamma_w}{\gamma_d}-1=\frac{2.65\times9.81}{15.1}-1=\boxed{0.722}.$$
Part (b) — porosity.
$$n=\frac{e}{1+e}=\frac{0.722}{1.722}=\boxed{41.9\%}.$$
Part (d) — moisture content. With $\gamma=\gamma_d(1+w)$,
$$w=\frac{\gamma}{\gamma_d}-1=\frac{17.0}{15.1}-1=\boxed{12.6\%}.$$
Part (c) — degree of saturation. From $wG_s=Se$,
$$S=\frac{wG_s}{e}=\frac{0.126\times2.65}{0.722}=\boxed{46.2\%}.$$
Only 46% of the void space is filled with water, so the soil is well above the water table — the "natural" state here is moist, not saturated.
Part (e) — buoyant unit weight. The buoyant (submerged) unit weight is a property of the soil skeleton once fully saturated at this SAME void ratio (i.e. if this soil were below the water table), $\gamma_b=\gamma_{sat}-\gamma_w$, which simplifies to
$$\gamma_b=\frac{(G_s-1)\gamma_w}{1+e}=\frac{(2.65-1)\times9.81}{1.722}=\boxed{9.40\ \text{kN/m}^3}.$$
Check: part (e) reports the buoyant unit weight the SAME soil skeleton would have if submerged (e unchanged) — the standard interpretation of "buoyant unit weight" for a soil described only in its unsaturated natural state, since $\gamma_b$ is not itself a natural-state quantity (S=46.2% here) but a property needed for effective-stress calculations below a water table.