16-Civ-B3 Geotechnical Design · December 2015
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
Paper format. Professional Engineers Ontario / Engineers Canada National Examinations, December 2015 — 98-Civ-B3 Geotechnical Design. Three hours, OPEN BOOK, any non-communicating calculator. Section A carries five discussion questions of 7 marks each (answer any four); Section B carries four design questions of 24 marks each (answer any three); the examinable total is 4 × 7 + 3 × 24 = 100 marks. All nine questions are worked below, because the set is a study resource rather than a timed attempt.
Reference texts (98-Civ-B3 / 16-Civ-B3 Geotechnical Design).
Sources of design charts and assumed values (page-1 Note 6). Note 6 of this paper requires the candidate to identify the source of every design chart used and of every value assumed in the absence of data. They are named where used and collected here:
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.
Recommendation. Support the structure on straight-shafted or belled drilled piers (cast-in-place concrete caissons) founded in the sand below the expansive clay, with the pier shafts sleeved or slip-coated through the active zone, tied together by grade beams cast on a void form so that they bear on nothing, and with all ground-supported floor slabs either structurally suspended over a void or accepted as sacrificial. This is the standard Canadian solution for a substantial structure over a shallow expansive deposit, and it is what CFEM recommends where the swelling soil is thin enough to be penetrated economically.
Why the obvious alternatives fail. The governing problem here is not bearing capacity and it is not settlement; it is differential vertical movement driven by moisture change. A highly expansive clay changes volume with water content, and water content changes seasonally at the perimeter, permanently under a heated slab, and catastrophically if a service leaks or landscape irrigation is installed. The movement is seasonal at the edges and cumulative in the centre, and it is measured in tens of millimetres. A conventional spread footing at, say, 1.5 m depth sits inside that active zone: it will be lifted in a wet cycle, dropped in a dry cycle, and the differential between a shaded north perimeter and a heated interior column will distort the frame far beyond anything the structure can tolerate. A raft is better because it bridges local variation, but a stiffened raft thick enough to resist the centre-heave and edge-lift bending moments generated by a highly expansive clay across a shopping-centre footprint is very expensive, and it does not remove the movement — it only makes the movement uniform enough to survive, which is a bet on the moisture regime staying uniform. It is a defensible solution for a small, single-storey, lightly loaded building, not for a multi-storey complex with column loads and a long design life. Removing and replacing 5 m of clay under a large footprint is technically valid and is sometimes done for roads, but the excavation volume, the disposal of a problem soil and the dewatering make it uncompetitive under a building.
Why drilled piers work. Piers carry the load past the entire active zone into a sand that does not change volume with water content, so the founding level is stable by construction. The sand is described as very deep, so end bearing is reliable and a belled base can develop a large capacity in a single element; where the sand is dense the bell may be unnecessary and a straight shaft with side resistance in the sand will do. Crucially, the design must then deal with the one mechanism that still couples the structure to the clay: uplift by shaft heave. When the clay swells it grips the pier and drags it upward, mobilising a tensile force over the whole thickness of the active zone. The design consequences are as follows.
Investigation required to complete the design. Swell–consolidation oedometer tests to obtain the swelling pressure and the free-swell strain, Atterberg limits and clay-fraction data to classify the expansive potential, natural water-content profiles in both a wet and a dry season to establish the depth of the active zone, and confirmation by borehole or CPT that the sand is continuous and competent at the founding level.