IS EN ISO 22282-2 and IS EN ISO 22282-3 define the framework for water permeability tests in geotechnical investigation, and in Celbridge these standards are not optional, they are essential. The town sits on the northern edge of the Carboniferous limestone plain where glacial till deposits overlay a karstified bedrock aquifer. This geological sequence, shaped by the Liffey valley and post-glacial drainage, means that excavation design or dewatering without a field-measured hydraulic conductivity value is a gamble. We run Lefranc tests in soil horizons and Lugeon tests in fractured rock because the interface between till and limestone here controls groundwater flow. A simple lab permeameter test on a disturbed sample will miss the secondary permeability that dominates the real behaviour of this ground.
A single Lugeon value of 3 Lu at 15 m depth can mean the difference between sump pumping and a full wellpoint dewatering system.
