One of the most common oversights we see in Belfast is assuming that the permeability of the local glacial till is uniform enough to skip site-specific testing. Contractors will often bank on a desk study value for hydraulic conductivity, only to find groundwater pouring into an excavation at rates their sump pumps simply can't handle. The city sits on a complex mosaic of lodgement till, glaciofluvial sands, and weathered Mercia Mudstone, meaning two boreholes fifty metres apart can yield completely different permeability characteristics. A properly executed field permeability test removes the guesswork from dewatering design, allowing you to size pumps, specify cutoff walls, or design grouting programmes based on what the ground actually does rather than what the textbook says it should do. We run both the Lefranc method for variable-head checks in soil and the Lugeon test in fractured rock, following BS 5930:2015 procedures to give you defensible, repeatable data for your temporary works and permanent drainage strategies.
A single Lugeon test in fractured Mercia Mudstone tells you more about real groundwater behaviour than a dozen lab permeameter tests on intact core.
