AbstractTidal fluctuation is shown to affect the piezometer readings taken in a nearshore aquifer around a working nuclear power station. Continuous monitoring of a network of 40 piezometers provided relations between the tidal cycle and the piezometer readings. These relations can be expressed in terms of a time lag and amplitude scaling factor. Using these parameters, tidal interference was filtered from the day‐to‐day piezometer readings. The early detection of ground‐water drawdown below the working station caused by construction of a new nuclear power station on an adjacent site could thus be achieved.In parallel with the field work, the theoretical relationship between the tide and piezometric response was shown to be of the same form as that observed in the field. Values of the aquifer characteristics could then be deduced and compared with those measured in conventional pumping tests. The transmission of the pressure oscillation is shown to be faster in areas of higher permeability and in the deeper parts of the aquifer. This second effect is thought to be caused by the presence of the phreatic su
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