The first thing you notice on a Blenheim site with deep vibratory compaction is the rig itself—a crawler-mounted leader supporting a long, slender vibroflot that hums at 1800 rpm. In the Wairau Valley, we typically deploy electrically powered units with variable frequency drives, allowing the operator to adjust eccentric moment as the probe descends through layered alluvium. The real craft lies in reading the ammeter in real time. A sudden drop in current signals a loose pocket; a steady climb means the soil fabric is densifying. In Blenheim’s post-glacial gravels, achieving consistent cone resistance often requires a two-pass offset grid. The proximity to the Wairau Aquifer, which supplies the town’s drinking water, means we also monitor pore pressure dissipation carefully—something the CPT test helps verify before and after treatment runs.
In Blenheim’s gravelly alluvium, a two-pass vibrocompaction grid with offset spacing often raises SPT N-values from single digits to over 25 in the critical upper 12 metres.
