The implementation of Eurocode 7 (BS EN 1997-1:2004+A1:2013) for tunnel design in Ashford demands a rigorous understanding of the local Weald Clay. This formation, which underlies much of the town and its planned infrastructure extensions near Junction 9 of the M20, is notorious for its high plasticity and low bearing capacity when saturated. Standard site investigation approaches often underestimate the time-dependent settlement and the squeezing pressures exerted on temporary linings. Our laboratory testing programme, compliant with BS 5930:2015+A1:2020, quantifies the undrained shear strength profile and the consolidation characteristics that govern face stability. When the alignment crosses areas of Head deposits overlying the clay—common in the Stour Valley to the north of the town centre—we integrate in-situ permeability testing to define the groundwater regime with precision, a critical input for finite element models of tunnelling-induced settlement.
In Ashford's Weald Clay, the difference between designing for peak strength versus residual strength can mean the difference between a controlled settlement trough and a catastrophic face collapse.
