Robison W L, Noshkin V E
Lawrence Livermore National Laboratory, CA 94551-0808, USA.
Sci Total Environ. 1999 Sep 30;237-238:311-27. doi: 10.1016/s0048-9697(99)00145-x.
Between June 1946 and October 1958, Enewetak and Bikini Atolls were used by the US as testing grounds for 66 nuclear devices. The combined explosive yield from these tests was 107 million t (million t TNT equivalents). This testing produced close-in fallout debris that was contaminated with quantities of radioactive fission and particle activated products, and unspent radioactive nuclear fuel that entered the aquatic environment of the atolls. Today, the sediments in the lagoons are reservoirs for tens of TBq of the transuranics and some long-lived fission and activation products. The larger amounts of contamination are associated with fine and coarse sediment material adjacent to the locations of the high yield explosions. Radionuclides are also distributed vertically in the sediment column to various depths in all regions of the lagoons. Concentrations greater than fallout background levels are found in filtered water sampled over several decades from all locations and depths in the lagoons. This is a direct indication that the radionuclides are continuously mobilized to solution from the solid phases. Of particular importance is the fact that the long-lived radionuclides are accumulated to different levels by indigenous aquatic plants and organisms that are used as food by resident people. One might anticipate finding continuous high contamination levels in many of the edible marine organisms from the lagoons, since the radionuclides associated with the sediments are not contained and are available to the different organisms in a relatively shallow water environment. This is not the case. We estimate that the radiological dose from consumption of the edible parts of marine foods at Enewetak and Bikini is presently approximately 0.05% of the total 50-year integral effective dose from all other exposure pathways that include ingestion of terrestrial foods and drinking water, external exposure and inhalation. The total radiological dose from the marine pathway is dominated by the natural radionuclides, 210Po and 210Pb. Man-made radionuclides presently contribute < 0.3% of the dose from these natural radionuclides in the marine food chain and within approximately 90 years only 0.15%.
1946年6月至1958年10月期间,美国将埃尼威托克环礁和比基尼环礁用作66个核装置的试验场。这些试验的总爆炸当量为1.07亿吨(亿吨TNT当量)。这种试验产生了近距离沉降碎片,这些碎片被大量放射性裂变和粒子活化产物以及未消耗的放射性核燃料污染,这些物质进入了环礁的水生环境。如今,环礁湖中的沉积物是数十太贝克超铀元素以及一些长寿命裂变和活化产物的储存库。大量的污染物与高当量爆炸地点附近的细颗粒和粗颗粒沉积物有关。放射性核素在沉积物柱中也垂直分布到环礁湖所有区域的不同深度。在环礁湖所有位置和深度数十年间采集的过滤水中,都发现其浓度高于沉降物背景水平。这直接表明放射性核素在不断地从固相转移到溶液中。特别重要的是,长寿命放射性核素被当地水生植物和生物积累到不同水平,而这些植物和生物是当地居民的食物来源。有人可能会预期,环礁湖中许多可食用海洋生物会持续处于高污染水平,因为与沉积物相关的放射性核素没有被截留,并且在相对较浅的水环境中可供不同生物利用。但实际情况并非如此。我们估计,目前在埃尼威托克和比基尼食用海洋食物可食用部分所接受的辐射剂量,约占包括摄入陆地食物和饮用水、外部照射和吸入在内的所有其他暴露途径50年累计有效剂量总量的0.05%。海洋途径的总辐射剂量主要由天然放射性核素210钋和210铅构成。目前,人造放射性核素在海洋食物链中占这些天然放射性核素剂量的比例不到0.3%,在大约90年内仅占0.15%。