Why asphalt fails
How Freeze-Thaw Cycles Break Down Asphalt in Waterloo Region
Freeze-thaw cycles break asphalt by letting water in, freezing it and then removing the support it leaves behind. A Waterloo Region winter swings above and below 0 C dozens of times, and each swing repeats the damage.
The cycle runs in four stages. Most repair calls we get in March and April are stage four on a driveway or lot that showed stage one the autumn before.
1. Water gets in
Rain and snowmelt enter through open cracks, seams and porous, oxidized asphalt. On the clay and silt till under much of Kitchener, that water has nowhere to drain, so it sits in the base.
2. Ice lifts the surface
Water expands about 9% as it freezes, pushing the asphalt up and widening every crack it fills. Frost reaches about 1.2 m (4 ft) deep here, far below any driveway base, so drainage matters more than depth.
3. The thaw leaves a void
When the ice melts, the lifted asphalt settles onto base that is now wet, loose and weaker than before. The surface looks intact but is bridging a soft spot.
4. Traffic breaks through
Tires flex the unsupported asphalt until it cracks into pieces and pops out as a pothole. Road salt adds to the damage by speeding up ravelling on unsealed, grey asphalt.
Soil changes the pace. Sandy ground on the Waterloo Moraine under west Kitchener and Waterloo drains faster and heaves less, while clay neighbourhoods see the same cracks turn into potholes within one or two winters.
Breaking the cycle at stage one is cheap: sealed cracks and a sealed surface keep water out of the base. Every stage after that costs more to fix.