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Unsaturated Soil Analysis for Toronto Foundations

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The difference between building on the sandy lacustrine deposits of Scarborough Bluffs versus the dense glacial till of North York is night and day in terms of unsaturated behavior. In Toronto, where the water table can sit 12 to 18 metres below grade in the upland areas, the vadose zone governs foundation performance. We see this especially on projects near the Don Valley or along the Humber River, where till crusts develop high matric suction during dry summers. That suction holds the soil together, but once you excavate or saturate it during spring thaws, the strength drops fast. That is why we pair our unsaturated soil analysis with a resistivity survey (SEV) to map moisture variability across the site before designing the sampling grid.

Illustrative image of Suelos no saturados in Toronto
In Toronto's glacial till, a 50 kPa drop in matric suction can reduce undrained shear strength by nearly 40 percent during wet seasons.

Methodology and scope

ASTM D5298 (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) governs the filter paper method we use to measure matric suction, and for Toronto's glacial till we also apply the axis-translation technique per ASTM D6836. The relevance here is high: the city's soils are typically overconsolidated, unsaturated, and prone to swelling when wetted — particularly the shale-derived clays along the Lake Ontario shoreline. Our protocol includes constructing soil-water characteristic curves (SWCC) for each stratigraphic unit, then using Fredlund's equations to model shear strength changes with saturation. We always run volumetric shrinkage tests on the same samples because the transition from unsaturated to saturated can trigger differential movement in slab-on-grade foundations. For deeper insight we also perform a full study of soil mechanics to correlate suction profiles with bearing capacity across the site.
Technical reference image — Toronto

Local considerations

A common error we see in Toronto is that contractors assume the stiff brown till near the surface behaves the same when fully saturated. They skip the unsaturated soil analysis, pour a slab in late summer, and by the following spring the clay till wets up, loses suction, and the slab cracks from differential heave. We had one job in Etobicoke where the owner tried to save CA$3,000 by skipping suction tests — ended up spending CA$38,000 on slab jacking and crack repairs. The real kicker is that the collapse potential was moderate at the site, and a simple double-oedometer test would have caught it before concrete ever touched the ground.

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Technical parameters

ParameterTypical value
Matric suction range (filter paper method)0 – 1500 kPa (ASTM D5298 (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4))
SWCC fitting modelFredlund & Xing (1994) – van Genuchten (1980)
Collapse potential (double oedometer)ASTM D5333 (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) — classification: slight to moderate
Swelling pressure (oedometer)ASTM D4546 (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) — 20 to 150 kPa typical for Toronto clay till
Volumetric shrinkage (bar linear)ASTM D4943 — <4% linear for low-plasticity till
Hydraulic conductivity (unsaturated)k(ψ) estimated via SWCC — range 10⁻⁷ to 10⁻¹¹ m/s

Associated technical services

01

Matric Suction Profiling

In-situ suction measurements using thermal conductivity sensors (ASTM D5298 (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4)) at 0.5 m depth intervals down to 5 m. Includes laboratory SWCC determination for the two dominant soil layers. Ideal for low-rise residential slabs and basement walls.

02

Collapse & Swell Assessment

Double-oedometer collapse tests (ASTM D5333 (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4)) plus free-swell oedometer (ASTM D4546 (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4)) on undisturbed tube samples from the till and lacustrine clay. Provides collapse index and swelling pressure for foundation design. Recommended for mid-rise buildings with shallow footings.

03

Full Unsaturated Shear Strength

Triaxial CU tests at three matric suction levels (0, 50, 150 kPa) using axis-translation. Yields the phi-b parameter and the extended Mohr-Coulomb envelope. Required for slope stability analysis in ravines or deep excavations where the water table fluctuates seasonally.

Applicable standards

ASTM D5298 (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (filter paper suction measurement), ASTM D6836 (SWCC via axis-translation technique), ASTM D5333 (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (collapse potential of soils), ASTM D4546 (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (CFEM Ch 4) (swelling pressure of cohesive soils), NBCC 2020 — Part 4: Foundations and geotechnical design

Frequently asked questions

How is unsaturated soil analysis different from standard consolidation testing?

Standard consolidation tests assume the soil is fully saturated and pore pressures dissipate under load. Unsaturated analysis adds the dimension of matric suction — a negative pore pressure that holds grains together. In Toronto's till, this suction can be 50–150 kPa in summer and near zero in spring, so we measure it separately and model its effect on strength and volume change using the SWCC and Fredlund's equations.

What is the typical cost range for an unsaturated soil analysis in Toronto?

For a standard residential lot with 3 suction profiles and collapse/swell tests, the cost ranges between CA$1,220 and CA$4,140 depending on site access, number of samples, and whether triaxial testing is included. The full unsaturated shear strength package for a deep excavation or ravine site falls at the upper end of that range.

Which Toronto neighbourhoods are most affected by unsaturated soil issues?

The reference range for this service in Toronto is CA$1.220 - CA$4.140. The final price depends on the project scope and volume.

Location and service area

We serve projects across Toronto and its metropolitan area.

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