Cardiff grew fast during the 19th-century coal boom, turning tidal marshes and reclaimed docklands into the city centre we know today. That history matters because much of the ground beneath the urban core consists of soft alluvial clays, glacial tills, and made ground from old railway sidings. For any project here, knowing the drained shear strength of those materials is essential. We run the direct shear test in Cardiff as a reliable way to obtain cohesion and friction angle values for slope stability and foundation design. The test follows BS 1377-7:1990, giving engineers parameters they can trust when checking bearing capacity or lateral earth pressures. Before we set up the shear box, we often recommend a complementary asentamiento differential analysis to identify potential differential movements in layered profiles.

In Cardiff's alluvial clays, the direct shear test provides effective stress parameters that are critical for slope stability and foundation design under drained conditions.