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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)

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
Natural (moist) unit weight$\gamma$17.0 kN/m³
Dry unit weight$\gamma_d$15.1 kN/m³
Specific gravity of solids$G_s$2.65

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.

  1. Part (a) — void ratio from the dry unit weight. Since $\gamma_d=\dfrac{G_s\gamma_w}{1+e}$, $$e=\frac{G_s\gamma_w}{\gamma_d}-1=\frac{2.65\times9.81}{15.1}-1=\boxed{0.722}.$$
  2. Part (b) — porosity. $$n=\frac{e}{1+e}=\frac{0.722}{1.722}=\boxed{41.9\%}.$$
  3. Part (d) — moisture content. With $\gamma=\gamma_d(1+w)$, $$w=\frac{\gamma}{\gamma_d}-1=\frac{17.0}{15.1}-1=\boxed{12.6\%}.$$
  4. 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.
  5. 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.
QuantityValue
(a) Void ratio, $e$0.722
(b) Porosity, $n$41.9%
(c) Degree of saturation, $S$46.2%
(d) Moisture content, $w$12.6%
(e) Buoyant unit weight, $\gamma_b$9.40 kN/m³
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