The National Building Code of Canada sets the baseline, but here in St Albert the real work starts when you hit the glacial stratigraphy. Our team deals with the lacustrine clays and silty tills that define the Sturgeon River valley every day. Stone column design in this part of Alberta has to account for frost penetration reaching 2.4 meters and a seasonal high water table that shifts the effective stress faster than standard assumptions predict. When a developer calls us about a low-rise commercial pad near Ray Gibbon Drive, we already know the overconsolidated crust is thinner than the borehole logs from twenty years ago suggest. We pair the CPT test with laboratory consolidation data to calibrate the settlement reduction factor instead of relying on generic Priebe charts alone, because the laminated silts here behave nothing like the uniform sands those charts were built for.
A stone column is only as good as the triaxial test on the local aggregate you feed into the Priebe method.



