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16-Civ-A4 Geotechnical Materials and Analysis · December 2015

Question 3 of 6: Effective vertical stress in a clay layer over an artesian sand

Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)

Notes on this paper

Paper format: National Examination 98-Civ-A4 Geotechnical Materials and Analysis — December 2015. Closed book, 3 hours, 100 marks. Six questions, answer all. Newmark and rectangular m–n influence charts and a formula sheet are provided at the back of the paper.

Reference texts: Das & Sobhan, Principles of Geotechnical Engineering (Cengage); Knappett & Craig, Craig’s Soil Mechanics; Holtz, Kovacs & Sheahan, An Introduction to Geotechnical Engineering. Canadian practice: effective-stress, seepage and consolidation methods as summarised in the Canadian Foundation Engineering Manual (CFEM, 4th ed.).

Question 3: Effective vertical stress in a clay layer over an artesian sand (10 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. Profile from ground level (GL): upper sand 0–4 m, clay 4–8 m, lower (artesian) sand 8–12 m. Water table 2 m below GL; lower sand piezometric surface 4 m above GL.

Given data
QuantityValue
Upper-sand unit weight, above WT16.5 kN/m3
Sand saturated unit weight19 kN/m3
Clay saturated unit weight20 kN/m3
Water table depth2 m below GL
Artesian piezometric surface4 m above GL
Unit weight of water, $\gamma_w$9.81 kN/m3

Find. The effective vertical stress $\sigma'_v$ at the top of the clay (depth 4 m) and at the bottom of the clay (depth 8 m).

Sand γ=16.5 / 19Clay γsat=20Sand (artesian) γsat=19GL (top of upper sand)WT (2 m)top of claybase of claypiezometricsurface (+4 m)
Figure 3.1 — layered profile: water table 2 m down, lower sand artesian (piezometric surface 4 m above GL).

Approach. Build the total vertical stress by summing $\gamma\,z$ layer by layer, obtain the pore pressure separately (hydrostatic from the water table in the upper sand; from the artesian piezometric surface at the base of the clay), and subtract: $\sigma'_v = \sigma_v - u$.

  1. Total stress at the top of the clay (z = 4 m). The upper sand is moist over the top 2 m and saturated over the next 2 m: $$\sigma_v = (2)(16.5) + (2)(19) = 33 + 38 = 71\ \text{kPa}.$$
  2. Pore pressure at the top of the clay. The upper sand is in free hydrostatic communication with the water table 2 m above this level: $$u = (4-2)\,\gamma_w = (2)(9.81) = 19.62\ \text{kPa}.$$
  3. Effective stress at the top of the clay. $$\sigma'_{v,\text{top}} = 71 - 19.62 = \boxed{51.4\ \text{kPa}}.$$
  4. Total stress at the base of the clay (z = 8 m). Add the 4 m clay column: $$\sigma_v = 71 + (4)(20) = 71 + 80 = 151\ \text{kPa}.$$
  5. Pore pressure at the base of the clay. Here the clay is in contact with the artesian lower sand, whose piezometric surface stands 4 m above GL. The pressure head at this point is the height of the piezometric surface above it, $8 + 4 = 12$ m: $$u = (12)(9.81) = 117.72\ \text{kPa}.$$
  6. Effective stress at the base of the clay. $$\sigma'_{v,\text{base}} = 151 - 117.72 = \boxed{33.3\ \text{kPa}}.$$
Final results — Question 3
Location$\sigma_v$ (kPa)$u$ (kPa)$\sigma'_v$ (kPa)
Top of clay (4 m)71.019.651.4
Base of clay (8 m)151.0117.733.3

Note that the effective stress decreases from 51.4 kPa at the top of the clay to 33.3 kPa at its base, even though the total stress rises by 80 kPa. The artesian head drives an upward pore-pressure gradient across the clay, so the clay near the lower sand is the most vulnerable to loss of effective stress (and to heave if the artesian head were to rise).