A lot of what we see in Ottawa geotechnical reports underestimates the complexity of the local overconsolidated clays until a proper triaxial test is run. You can have decent SPT numbers in the field and still end up with unexpected settlement because the stress history of Champlain Sea deposits isn't obvious from index tests alone. The atterberg limits lab work gives you the classification, sure, but for the effective friction angle and undrained shear strength that actually drive deep foundation design—or the stability analysis on an excavation near the Rideau Canal—the triaxial test is non-negotiable. Our team works with local consulting firms who know that a consolidated-undrained test with pore pressure measurement tells a different story than a quick unconfined compression on a Shelby tube sample; we see it every season, especially in the softer zones east toward Orleans where the clay sensitivity runs high.
A consolidated-undrained triaxial test with pore pressure measurement on Leda clay reveals strength ratios that index tests simply can't predict.



