Further studies of the distribution of technetium-99 and caesium-137 in UK and European coastal waters
Data on the temporal and spatial variations of 99Tc and 137Cs in UK coastal waters are provided from surveys carried out over the period 1993–1998; prior to and post the discharge of elevated quantities of 99Tc from the nuclear fuel reprocessing plant at Sellafield (Cumbria, UK). 99Tc seawater conce...
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Veröffentlicht in: | Continental shelf research 2002-06, Vol.22 (10), p.1417-1445 |
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Zusammenfassung: | Data on the temporal and spatial variations of
99Tc and
137Cs in UK coastal waters are provided from surveys carried out over the period 1993–1998; prior to and post the discharge of elevated quantities of
99Tc from the nuclear fuel reprocessing plant at Sellafield (Cumbria, UK).
99Tc seawater concentrations in the Irish Sea increased by more than an order of magnitude within the study period concomitant with the increase in discharges.
137Cs discharges were relatively low (∼0.3% of their peak values in the 1970s). Simplistically, the
137Cs distribution reflected varying hydrographic conditions superimposed upon the residual concentrations of a system approaching steady state. Differences between the
137Cs/
99Tc ratio in Sellafield discharges and seawater indicate that
137Cs remobilisation, from sediments contaminated by large discharges in the 1970s, is presently the predominant (∼90%) source term to the water column. The
137Cs/
99Tc ratio in the Irish Sea decreased significantly within the period of these surveys (e.g. reduced from ∼14 in 1993 to 0.4 in 1996, within the vicinity of Sellafield). However, it is difficult to extrapolate this information to assess the contribution from Sellafield in distant waters because the low levels of
137Cs are continuously perturbed by additional inputs during transit (e.g. remobilisation from sediments outside the Irish Sea). Examination of
99Tc data for the North Sea indicates that the leading edge of the first EARP pulse, entering via the Scottish coastal current, may have migrated to the limit of the current flowing south along the British coastal margin within 9 months. The estimated transfer factor (TF) for Sellafield discharges in this current is 52
Bq
m
−3/PBq
annum
−1 with transit times from Sellafield to the Pentland Firth and Lowestoft of ∼9 and ∼24 months, respectively. These transit times, derived from the
99Tc data, are significantly shorter than previous estimates based on
137Cs and
90Sr data from the 1970s and 1980s. |
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ISSN: | 0278-4343 1873-6955 |
DOI: | 10.1016/S0278-4343(02)00021-3 |