18-Env-A3 Geotechnical and Hydrogeological Engineering · December 2015
Question 5 of 6: Rankine Active Force — Two-Layer Backfill with Water Table and Surcharge
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
Notes on this paper
National Exams — December 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, compaction, lateral earth pressure and retaining-wall stability chapters; Craig & Knappett, Craig's Soil Mechanics (8th ed.) — seepage/flow-net theory and Rankine earth-pressure cross-reference; Freeze & Cherry, Groundwater (1979) — Darcy's law, anisotropic layered media and the Dupuit–Thiem equation for radial flow to a well.
Question 5: Rankine Active Force — Two-Layer Backfill with Water Table and Surcharge (20 marks)
Check: the source prints the surcharge as $q=15\ \text{kN/m}^3$, but a surcharge is a pressure (force per area), not a unit weight — kN/m³ is dimensionally impossible for a surface load. This is read as the standard convention $q=15\ \text{kN/m}^2=15\ \text{kPa}$.
Given.
Given data
Quantity
Symbol
Value
Total wall height
$H$
6 m
Depth to water table
$H_1$
2 m
Unit weight above WT
$\gamma_1$
16 kN/m³
Saturated unit weight below WT
$\gamma_2$
19 kN/m³
Friction angle above / below WT
$\phi_1,\phi_2$
32°, 36°
Surface surcharge
$q$
15 kPa
Find. (a) Rankine active force per unit length, $P_a$; (b) height of the resultant above the wall base.
Effective (Rankine) active-earth-pressure diagram in orange, hydrostatic pore-water pressure in blue — both plotted to scale against the wall face.
Approach. Compute each layer's own $K_a$ from its own $\phi$, apply it to the EFFECTIVE vertical stress at that depth (using the submerged unit weight $\gamma_2'=\gamma_2-\gamma_w$ below the water table), add the hydrostatic pore-water pressure separately, decompose the resulting diagram into elementary rectangles/triangles, then sum forces and take moments about the base.
Lateral effective pressures — note the JUMP at the water table since $K_a$ changes even though $\sigma'_v$ is continuous:
$$\sigma'_{h1,\text{top}}=K_{a1}(15.0)=4.61,\quad \sigma'_{h1,\text{bot}}=K_{a1}(47.0)=14.44\ \text{kPa (layer 1)},$$
$$\sigma'_{h2,\text{top}}=K_{a2}(47.0)=12.20,\quad \sigma'_{h2,\text{bot}}=K_{a2}(83.76)=21.75\ \text{kPa (layer 2)}.$$
Decompose into five elementary areas and sum. Layer 1 (surcharge rectangle + self-weight triangle), layer 2 (carried-over rectangle + incremental triangle), and the water-pressure triangle over the full 4 m submerged depth:
$$F_1=9.22,\ F_2=9.83,\ F_3=48.81,\ F_4=19.09,\ F_w=78.48\ \text{kN/m},$$
$$P_a=F_1+F_2+F_3+F_4+F_w=\boxed{165.4\ \text{kN/m}}.$$
(b) Location of the resultant — take moments of each shape's own centroid height above the base ($y_1=5.00,\ y_2=4.667,\ y_3=2.00,\ y_4=y_w=1.333$ m):
$$\bar y=\frac{F_1y_1+F_2y_2+F_3y_3+F_4y_4+F_wy_w}{P_a}=\frac{319.5}{165.4}=\boxed{1.93\ \text{m above the base}}.$$