Comparing a site in Sahali, perched on compact glacial till, to one in Valleyview, sitting atop looser fluvial sediments along the South Thompson River, highlights the stark contrasts we manage daily in Kamloops. The city’s semi-arid climate—averaging just 278 mm of precipitation annually—masks a complex subsurface shaped by glacial retreat and river migration. Designing vibrocompaction here means reading that history correctly. We apply energy-based densification logic rooted in field response, not generic charts, because the transition from dense till to liquefiable alluvium can happen within a single city block. This variability demands a ground improvement approach tailored precisely to local depositional sequences, and our triaxial testing program provides the critical strength parameters needed before any vibro treatment is finalized.
Achieving a 15% to 25% increase in relative density with vibrocompaction is routine in Kamloops sands, but only if the grain-size distribution confirms less than 12% fines.
