Accumulation, solid partitioning and remobilisation of 99Tc in subtidal and intertidal sediments in the Irish Sea
Autor: | Paul Finegan, Peter I. Mitchell, Peter J. Kershaw, Aurélien Gouzy, L. León Vintró, Julie Lucey, D. Boust |
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Přispěvatelé: | School of Physics, University College Dublin [Dublin] (UCD), Laboratoire de Radioécologie de Cherbourg-Octeville (LRC), Institut de Radioprotection et de Sûreté Nucléaire (IRSN) |
Jazyk: | angličtina |
Rok vydání: | 2009 |
Předmět: |
010504 meteorology & atmospheric sciences
[SDV]Life Sciences [q-bio] dissolution 010501 environmental sciences mudstone Sellafield Oceanography 01 natural sciences deposition Deposition (geology) beach profile intertidal environment Atlantic Ocean Seabed physical geography seafloor Outfall Geology Seafloor spreading Europe remobilization speciation (chemistry) fallout England chromatography geoaccumulation sequestration (chemistry) Intertidal zone Western Europe Irish Sea Aquatic Science Structural basin Marine pollution discharge cesium isotope subtidal environment 14. Life underwater reworking 0105 earth and related environmental sciences sediment pollution Sediment surficial sediment United Kingdom marine pollution technetium isotope homogeneity Cumbria fine grained sediment extraction Eurasia time series volatile element |
Zdroj: | Continental Shelf Research Continental Shelf Research, Elsevier, 2009, 29 (16), pp.1995-2010. ⟨10.1016/j.csr.2009.02.005⟩ |
ISSN: | 0278-4343 1873-6955 |
Popis: | Recent studies have shown that accumulation of 99 Tc in seabed sediments labelled by authorised radioactive liquid discharges into the NE Irish Sea from the Sellafield reprocessing complex is greater than previously thought. In this paper, new data on 99 Tc concentration profiles in subtidal and intertidal sediments from the eastern and western Irish Sea are provided with a view to elucidating the processes responsible for the incorporation and retention of 99 Tc in the seabed. The data show that substantial amounts of 99 Tc have accumulated in the fine-grained subtidal sediments off the Cumbrian coast, particularly after increased releases from Sellafield following the commissioning of the Enhanced Actinide Removal Plant (EARP) in 1994. In all the cores taken in this area, 99 Tc has been found to be present to depths in excess of 30 cm. Analysis of 137 Cs and 241 Am profiles, together with other supporting geochemical data, show a high degree of homogenisation of the sediments down to these depths as a result of physical and biological processes, and confirm that incorporation of 99 Tc into the sediment compartment is actually the result of mixing and reworking, rather than active sediment accumulation. In contrast, active deposition of material transported from this mixed pool of sediment appears to be the dominant mechanism controlling 99 Tc profiles in intertidal areas close to the Sellafield discharge outfall. Data obtained from the analysis of subtidal sediment cores from the western Irish Sea mud basin suggest that similar mixing processes to those occurring in the subtidal sediments of the eastern Irish Sea are also active in this area. Time-series data on 99 Tc concentrations in surficial sediments from this basin, gathered in the period 1988–2004, inclusive, show a clear increase in concentrations, by a factor of ∼2, between samples collected pre-EARP and post-EARP. The constancy of 99 Tc concentrations in surface sediments throughout the 1980s and the early-1990s suggests that little redissolution and export of 99 Tc occurred over this extended period. A similar observation applies to the post-EARP period, when concentrations remained relatively constant despite the reported steady decrease in 99 Tc concentrations in the overlying waters. This apparent lack of remobilisation is consistent with data from sequential extraction analyses, which indicate that the bulk of the 99 Tc is strongly bound to non-labile geochemical phases, with only a small proportion associated with exchangeable and acido-soluble phases. Further, these analyses show that 99 Tc is not associated with oxygen-sensitive and highly-reactive acid-volatile sulphides (AVS) to any significant extent. |
Databáze: | OpenAIRE |
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