New Westminster's pavement infrastructure contends with a complex geological legacy. The city sits at a dynamic interface where upland glacial till meets the compressible silts and clays of the Fraser River floodplain, a condition that the National Building Code of Canada (NBCC) specifically addresses for seismic and settlement-sensitive design. In our experience, a standard pavement section simply does not work here. The native soils vary dramatically within a few hundred meters, demanding a flexible pavement design approach that accounts for differential settlement and lateral spreading potential. Following CSA A23.3 and relevant ASTM standards, we focus on the structural number required to bridge these variable subgrades. A proper grain-size analysis becomes the foundational step, revealing the fines content that dictates drainage behavior and frost susceptibility beneath the asphalt layers.
A pavement section in New Westminster is only as reliable as its subgrade assessment; ignoring the local clay's shrink-swell potential can halve the design life.
