Sault Ste Marie sits on a mix of glacial till, lacustrine clay, and silty sand deposits left by the retreat of the Lake Superior lobe. Compacted subgrade here has to handle freeze-thaw cycles that reach 1.8 m depth, plus summer humidity pushing moisture back into the formation. We run the California Bearing Ratio test inside a controlled soak tank that simulates four days of saturation, because the worst case for any pavement in the Soo is spring break-up. The plunger load is read at 2.54 mm and 5.08 mm penetration and compared against the standard crushed-stone reference. For granular base courses we often pair the CBR with a grain size analysis to confirm the gradation envelope before the soaked strength is recorded.
Soaked CBR in the Soo's silty clays can drop by half compared to as-compacted — the lab soak reveals what spring will do.
