Ottawa sits on roughly 70 meters of sensitive Leda clay, a Champlain Sea deposit that has shaped every major underground project in the capital region since the 1960s. Our laboratory handles soil samples from Confederation Heights to Kanata, and the challenge is always the same: undisturbed strength drops dramatically once the clay structure is broken. We run the full suite of index and strength tests because no two boreholes in this city read the same. For deeper alignments, we pair routine classification with triaxial testing to capture the undrained shear strength profile that governs face stability. When the tunnel horizon dips into glacial till, we also cross-check with grain-size analysis to flag boulders and cobbles that can blind a TBM cutterhead overnight.
Ottawa's Leda clay loses over 80% of its undisturbed strength when remolded. That single fact drives every pore-pressure assumption in our tunnel face-stability models.


