The distribution of plutonium and americium in the sub-tidal sediments of the Irish Sea is described following major surveys in 1978, 1983, 1988 and 1995. Concentrations in surface sediments have declined near the source at Sellafield since 1988, Time-series of inter-tidal surface sediment concentrations are presented from 1977 onwards. revealing the importance of sediment reworking and transport in controlling the evolution of the: environmental signal. The surface and near-surface sediments, in the eastern Irish Sea 'mud-patch', are generally well mixed with respect to Pu (alpha) and Am-241 distributions but show increasing variability with depth-up to 4 orders of magnitude in concentration. The inventories of Pu-239,Pu-240 and Am-241 in the sub-tidal sediments have been estimated and compared with the reported decay-corrected discharges. These amounted to 360 and 545 TBq respectively, in 1995, about 60% of the total decay-corrected discharge. Part of the unaccounted fraction may be due to unrepresentative sampling of the seabed. It is speculated that some tens of TBq of plutonium and Am-241 reside undetected in the large volumes of coarse-grained, sub-tidal and inter-tidal sediment which characterise much of the Irish Sea. This has been due to the inability of the available corers to penetrate to the base of contamination in these mobile sediments. Further observations are needed to verify and quantify the missing amount. A budget of plutonium-alpha and Am-241 has been estimated based on published observations in the three main compartments: water column, sub-tidal and inter-tidal sediments. This amounts to 460-540 TBq and 575-586 TBq respectively, or 64-75% band 60 61%, of the decay-corrected reported discharge. Crown Copyright (C) 1999 Published by Elsevier Science Ltd. All rights reserved.