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Pu Isotopic Composition Indicates Its Sources and Environmental Changes in the Vicinity of Daya Bay Nuclear Power Plant

文献类型： 外文期刊

作者： Chen, Jisheng 1 ; Yang, Panpan 2 ; Bu, Wenting 1 ; Xiong, Ke 1 ; Wang, Cui 4 ; Yan, Xiuli 2 ; Liu, Yong 5 ; Wu, Peng 5 ; Wu, Junwen 2 ;

作者机构： 1.China Acad Engn Phys, Inst Nucl Phys & Chem, Mianyang 621900, Peoples R China

2.Shantou Univ, Guangdong Prov Key Lab Marine Disaster Predict & P, Shantou 515063, Peoples R China

3.Shantou Univ, Inst Marine Sci, Shantou 515063, Peoples R China

4.Minist Nat Resource, Inst Oceanog 3, Xiamen 361005, Peoples R China

5.Chinese Acad Fishery Sci, Minist Agr & Rural Affairs, South China Sea Fisheries Res Inst, Key Lab South China Sea Fishery Resources Exploita, Guangzhou 510300, Peoples R China

关键词： plutonium; Pu-240/Pu-239 atom ratio; Daya Bay; pacific proving ground; north equatorialcurrent

期刊名称：ACS EARTH AND SPACE CHEMISTRY （ 影响因子：2.9； 五年影响因子：3.1 ）

ISSN： 2472-3452

年卷期： 2025 年 9 卷 2 期

页码：

收录情况： SCI

摘要： The plutonium (Pu) isotopic compositions of surface sediments and two sediment cores from Daya Bay were measured by ICP-MS for the sake of investigating the sources of Pu and their historical evolution. The surface Pu-240/Pu-239 atomic ratios in Daya Bay are in the range of 0.247-0.287 (average = 0.264 +/- 0.011, n = 14), which are higher than the characteristic value of global fallout (similar to 0.178) and indicate the input from non-global fallout. Correspondingly, the Pu239+240 activities were in the range of 0.029-0.386 Bq kg(-1) (average = 0.197 +/- 0.091 Bq kg(-1), n = 14), and their spatial distribution shows relatively high Pu activity at the mouth and western part of Daya Bay, which is mainly attributed to finer particle sizes. The high Pu-240/Pu-239 atomic ratios were confirmed to be from the contribution to Pacific Proving Grounds (65% +/- 7%) transported via the Kuroshio current. There was no additional Pu input released from the normal operation of Daya Bay nuclear power plants. Additionally, the Pu chronology of the sediment cores showed that changes in the sedimentary environment impact the Pu isotopic content. The Advection-Diffusion Equation model was used to further evaluate and predict the vertical migration of Pu isotopes in Daya Bay, suggesting that the diffusion of Pu over time may impact its usefulness as a time marker. Finally, we provide a baseline value of Pu isotopes in Daya Bay for environmental risk assessments in the future.

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