What Makes a Road Last Through Ontario Freeze-Thaw
A road survives Ontario freeze-thaw when its base stays drained, its granular layers are thick enough, its subgrade is firm and its crown sheds water. When any one of those is missing, spring thaw finds it.
Around Guelph, frost typically reaches about 1.2 m (4 ft) deep in a normal winter. Water in the base and in silty clay subgrade freezes into ice lenses that lift the road, then thaws from the top down in March and April, leaving saturated soil with nowhere to drain.
That is when trucks punch through: the base is wet, the still-frozen layer below holds the water in, and the road loses much of its bearing strength until it dries. Municipalities post reduced load limits on rural roads each spring for the same reason.
- Water in the base: dirty granulars with too many fines hold water, and ditches shallower than the base cannot drain it.
- Weak subgrade: wet clay and silt pump up into the gravel under traffic unless a geotextile keeps them apart.
- Thin granular layers: 150 mm (6 in) of gravel over clay may survive cars, but not a loaded tri-axle in April.
- Poor crown: a flat road ponds water, while a 2 to 4% cross slope sends it to the ditch.