Running a CBR test in St. Albert means dealing with two very different soil profiles depending on which side of the Sturgeon River you’re on. Over in the older neighborhoods like Grandin and Braeside you’ll hit the glacial till fairly shallow—dense, silty clay with some sand lenses, and it usually delivers CBR values above 8% without much trouble. Cross the river into newer subdivisions around Jensen Lakes and suddenly you’re in lacustrine clay that turns to soup when it rains. We’ve seen soaked CBR values drop below 2% in that stuff, which changes your entire pavement design. That’s why we run both soaked and unsoaked specimens as standard practice—because the subgrade you compact in August is not the subgrade you’ll be driving on in April. Before committing to a structural section, many engineers pair the CBR data with a grain size analysis to confirm fines content, especially when the plasticity looks borderline for freeze-thaw durability. And where the subgrade is clearly problematic, we often recommend following up with stone columns as a ground improvement strategy before placing the base course.
A soaked CBR under 2% in St. Albert’s lacustrine clay means your pavement section just tripled in thickness—test it before you budget it.



