Unravelling 5 decades of anthropogenic 236U discharge from nuclear reprocessing plants

被引:35
|
作者
Castrillejo, Maxi [1 ]
Witbaard, Rob [2 ,3 ]
Casacuberta, Nuria [1 ,4 ]
Richardson, Christopher A. [5 ]
Dekker, Rob [2 ,3 ]
Synal, Hans-Arno [1 ]
Christl, Marcus [1 ]
机构
[1] Swiss Fed Inst Technol, Lab Ion Beam Phys, Otto Stern Weg 5, CH-8093 Zurich, Switzerland
[2] NIOZ Royal Netherlands Inst Sea Res, POB 59, NL-1790 AB Den Burg, Netherlands
[3] Univ Utrecht, POB 59, NL-1790 AB Den Burg, Netherlands
[4] Swiss Fed Inst Technol, Environm Phys, Inst Biogeochem & Pollutant Dynam, Univ Str 16, CH-8092 Zurich, Switzerland
[5] Bangor Univ, Sch Ocean Sci, Menai Bridge LL59 5AB, Anglesey, Wales
基金
英国生物技术与生命科学研究理事会;
关键词
Radioactive contamination; Uranium-236; Ocean circulation; Sclerochronology; Cerastoderma edule; Nuclear reprocessing; SOUTHERN NORTH-SEA; ENGLISH-CHANNEL; CERASTODERMA-EDULE; OCEANIC TRACER; COCKLE FISHERY; WADDEN SEA; URANIUM; SHELL; WATER; TERM;
D O I
10.1016/j.scitotenv.2020.137094
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Marine biogenic materials such as corals, shells, or seaweed have long been recognized as recorders of environmental conditions. Here, the bivalve Cerastoderma edule is used for the first time as a recorder of past seawater contamination with anthropogenic uranium, specifically U-236. Several studies have employed the authorized radioactive releases, including U-236, from nuclear reprocessing plants in La Hague, France, into the English Channel, and Sellafield, England, into the Irish Sea, to trace Atlantic waters and to understand recent climate induced circulation changes in the Arctic Ocean. Anthropogenic U-236 has emerged over recent years as a new transient tracer to track these changes, but its application has been challenged owing to paucity of fundamental data on the input (timing and amount) of U-236 from Sellafield. Here, we present U-236/U-238 data from bivalve shells collected close to La Hague and Sellafield from two unique shell collections that allow the reconstruction of the historical U-236 contamination of seawater since the 1960s, mostly with bi-annual resolution. The novel archive is first validated by comparison with well-documented U-236 discharges from La Hague. Then, shells from the Irish Sea are used to reconstruct the regional U-236 contamination. Apart from defining new, observationally based( 236)U input functions that will allow more precise tracer studies in the Arctic Ocean, we find an unexpected peak of U-236 releases to the Irish Sea in the 1970s. Using this peak, we provide evidence for a small, but significant recirculation of Irish Sea water into the English Channel. Tracing the 1970s peak should allow extending U-236 tracer studies into the South Atlantic Ocean. (C) 2020 The Authors. Published by Elsevier B.V.
引用
收藏
页数:9
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