In Pickering, we often see pavement failures that start not with traffic loads but with water trapped in the granular base. The city sits on a mix of Halton Till and glaciolacustrine deposits near the Lake Ontario shoreline. These silty clays hold moisture. When freeze-thaw cycles kick in during March, the subgrade loses strength fast. A flexible pavement design has to manage that seasonal swing. We model the structure using layered elastic theory and local CBR values, not generic tables. The AASHTO 93 method gives us a starting point, but we refine it with actual soil data from the site. For projects near the Rouge River floodplain, we also check the CBR road analysis to correlate field strength with lab results before finalizing the asphalt thickness.
A pavement is only as strong as its weakest springtime subgrade condition — that’s where we focus the geotechnical investigation in Pickering.
