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Sources of Anthropogenic 14 C to the North Sea

2004; Cambridge University Press; Volume: 46; Issue: 2 Linguagem: Inglês

10.1017/s0033822200035906

1945-5755

Pauline Gulliver, Gordon Cook, A.B. MacKenzie, Philip Naysmith, Robert F. Anderson,

Geology and Paleoclimatology Research

The Sellafield nuclear fuel reprocessing plant on the northwest coast of England is the largest source of anthropogenic radiocarbon to the UK coastal environment. In a mid-1990s study of 14 C distribution around the UK coast, the pattern of dilution with increasing distance from Sellafield appeared to be perturbed by anomalously high 14 C activities in marine biota in the coastal environment of northeast England. This present study was undertaken during 1998 and 1999 to determine whether this 14 C enhancement was due to Sellafield or the nuclear power plants on the east coast. Seawater, seaweed ( Fucus sp.), and mussel ( Mytilus edulis ) samples that were collected from the vicinity of the Torness and Hartlepool advanced gas-cooled reactor (AGR) nuclear power stations were all enhanced above the contemporary regional background activity derived from natural production and atmospheric nuclear weapons testing. We used previously published dilution factors and transfer times for 99 Tc between Sellafield and various points on the UK coast to determine likely Sellafield-derived 14 C contributions to the activities at the nuclear power plant sites. The results suggest that the activities observed at Torness, which are only marginally enhanced above the natural background activity, are possibly due to discharges from Sellafield; however, the significant 14 C enhancements at Hartlepool are not Sellafield-derived. Furthermore, since both reactors have the same fundamental design, the low activities at the Torness AGR imply that the activities at Hartlepool are not from the AGR, suggesting that there is an input of 14 C to the marine environment in the vicinity of Hartlepool which is probably non-nuclear-power related. However, there is no other authorized site in the area that could account for the observed 14 C enrichments; therefore, further research is required to ascertain the source of this 14 C.