Christchurch sits on a complex alluvial fan where the Waimakariri River has deposited interbedded sands, silts, and peats over millennia—a profile that liquefied extensively during the 2010-2011 Canterbury sequence. Designing a rigid pavement here means accepting that the subgrade will move. Rather than fighting it, our approach uses the slab’s flexural stiffness to bridge localised subsidence zones, distributing wheel loads across soft spots that would quickly rut a flexible pavement. The key lies in quantifying the subgrade’s post-liquefaction reconsolidation potential, which we assess through CPT testing to map the exact depth and thickness of liquefiable layers beneath the alignment. For industrial yards near the Heathcote River, where groundwater sits within 1.2 m of the surface, we often specify thickened edge beams and dowelled contraction joints to maintain load transfer even if the supporting soil loses 60% of its bearing capacity during a design-level event.
A rigid pavement in Christchurch doesn't just carry traffic—it's a structural slab designed to survive differential settlement of 150 mm without losing serviceability.
