On Dublin sites, the story of the ground is often written in the grain size. Boulder clay lodgement till covers much of the city, but it is rarely uniform—it shifts from sandy lenses near the coast to stony, matrix-supported diamicton only a mile inland. Our grain size analysis (sieve plus hydrometer) maps this full range, quantifying gravel, sand, silt, and clay fractions from the coarse fraction down to the colloidal 2-micron range, because a bulk description of 'brown boulder clay' is simply not enough to design a working drainage blanket, assess frost susceptibility, or confirm compliance with the TII Specification for Road Works Series 600 earthworks. We run the hydrometer test to ASTM D7928 procedure with sodium hexametaphosphate dispersion, which is critical for the marine-influenced clays found in the Docklands and along the Tolka estuary, and we cross-check the fines content with Atterberg limits testing whenever the hydrometer curve suggests a plasticity shift that could affect the Unified Soil Classification System (USCS) designation.
A single hydrometer curve on Dublin lodgement till reveals more about drainage and frost behaviour than twenty hand-auger descriptions combined.
