The bedrock beneath Portlaoise is predominantly Dinantian limestone, but what governs drainage on any given site is the overburden — a mixed mantle of glacial till and alluvial gravels deposited by the River Triogue. Permeability can vary by orders of magnitude within a single hectare. A borehole log tells you what the soil is; a field permeability test tells you how water actually moves through it. In our experience across the Midlands, assuming a textbook value for 'sandy gravel till' leads to oversized dewatering systems or, worse, flooded excavations. The Lefranc test gives us point measurements of hydraulic conductivity in soil, while the Lugeon test is the standard for assessing fracture flow in the underlying limestone — essential when a basement excavation in Portlaoise encounters weathered bedrock at 3 to 5 metres depth. We run these tests under constant or falling-head conditions, following IS EN ISO 22282 series, and report k-values directly usable for drain design or groundwater control planning.
A single field permeability test in Portlaoise till is worth more than ten desk-study estimates when groundwater is within excavation reach.
