School of Nuclear Science and Technology, University of South China, Hengyang, 421001, China.
School of Nuclear Science and Technology, University of South China, Hengyang, 421001, China.
J Environ Radioact. 2024 Feb;272:107364. doi: 10.1016/j.jenvrad.2023.107364. Epub 2024 Jan 2.
Plutonium-239 + 240 and Cs in the environment can usually be used to track the impact of nuclear activities on the environment, and have become important tools in environmental geochemical studies. In this study, nine sediment cores (E1-E9) in Lake East Dongting were collected and measured for the activity concentration of Pu, Cs and the atomic ratio of Pu/Pu, and then their vertical distribution characteristics were analyzed. The results show that: the activity concentrations of Cs and Pu in Lake East Dongting ranged from 5.26 ± 0.43 to 28.6 ± 2.23 Bq kg and 0.29 ± 0.02 to 1.37 ± 0.09 Bq kg, with an average of 7.48 ± 0.68 Bq kg and 0.39 ± 0.03 Bq kg, respectively. The atomic ratios of Pu/Pu are 0.168 ± 0.012-0.211 ± 0.015, which are basically consistent with the global atmospheric deposition. The vertical profiles of Cs and Pu in sediment cores show obvious single-peak distribution in E1-E6 and bimodal distribution in E7-E9. The results of sedimentation rates calculated by Cs and Pu method ranged from 0.59 cm y to 1.99 cm y with a mean of 1.18 cm y and 0.61 cm y to 2.18 cm y with a mean of 1.26 cm y. The inventories of Cs and Pu in nine sediment cores are 5.87-10.8 kBq m and 307-545 Bq m, which are about 8-14 and 9-15 times the inventory in the global average atmospheric deposition at the same latitude respectively. Comparing the results of the sedimentation rates and the inventories from different sampling points indicates that extreme climatic events and human activities have a significant impact on sediment environment of Lake East Dongting.
钚-239 和-240 以及环境中的铯通常可用于追踪核活动对环境的影响,并且已成为环境地球化学研究中的重要工具。本研究采集了东洞庭湖 9 个沉积物岩芯(E1-E9),测量了 Pu、Cs 的活度浓度以及 Pu/Pu 的原子比,并分析了它们的垂向分布特征。结果表明:东洞庭湖 Cs 和 Pu 的活度浓度范围分别为 5.26±0.43 至 28.6±2.23 Bq kg 和 0.29±0.02 至 1.37±0.09 Bq kg,平均值分别为 7.48±0.68 Bq kg 和 0.39±0.03 Bq kg。Pu/Pu 的原子比为 0.168±0.012-0.211±0.015,基本与全球大气沉降一致。沉积物岩芯中 Cs 和 Pu 的垂直分布呈明显的单峰分布,E1-E6 为双峰分布,E7-E9 为双峰分布。Cs 和 Pu 法计算的沉积速率范围分别为 0.59-1.99 cm y,平均值为 1.18 cm y 和 0.61-2.18 cm y,平均值为 1.26 cm y。9 个沉积物岩芯中 Cs 和 Pu 的含量分别为 5.87-10.8 kBq m 和 307-545 Bq m,分别约为全球同纬度平均大气沉降的 8-14 倍和 9-15 倍。比较不同采样点的沉积速率和储量结果表明,极端气候事件和人类活动对东洞庭湖的沉积物环境有显著影响。