One of the more costly mistakes we see in St. Albert subdivisions is a well-graded asphalt mat laid over a subgrade that nobody bothered to characterize beyond a quick visual check. Two winters later the road heaves, the surface cracks, and the pavement life drops by half. That outcome is entirely avoidable with a flexible pavement design grounded in local geotechnical data. The city sits on glaciolacustrine silts and clays deposited by the former Lake Edmonton, and these soils behave very differently from the glacial tills found just a few kilometres west. Our approach ties laboratory Atterberg limits and grain-size analysis to the structural number the pavement actually needs, so the cross-section reflects real subgrade conditions rather than a generic provincial default.
In St. Albert's glaciolacustrine clays, subgrade moisture control matters more than the asphalt thickness itself.



