In order to quantitatively evaluate and predict the behavior of the anthropogenic radionuclides, this study examined the spatiotemporal distributions and mass budgets of ¹³⁷Cs and ²³⁹,²⁴⁰Pu in the seas surrounding Korean Peninsula (i.e., the East/Japan Sea, the Yellow Sea, and the southern sea of Korea) from 2018 to 2024. Surface activities of ¹³⁷Cs ranged from 0.56 to 2.43 mBq kg⁻¹, while those of ²³⁹,²⁴⁰Pu ranged from 1.28 to 5.70 μBq kg⁻¹. ¹³⁷Cs showed a gradual decline over time, with surface distributions exhibiting slight spatial and temporal variations. The vertical distribution of ¹³⁷Cs showed surface or subsurface (< 100 m) peaks followed by a decrease with depth. In contrast, ²³⁹,²⁴⁰Pu activities were depleted near the surface and increased with depth, displaying a distinct maximum at mid-depth (750-1000 m). Mass balance calculations suggest the negative inventory change rates (dI/dt) across all regions, indicating net losses of ¹³⁷Cs primarily due to radioactive decay and particle scavenging. The corresponding residence times of ¹³⁷Cs were 70.7 ± 1.0 years in the East/Japan Sea, 40.1 ± 0.7 years in the Yellow Sea, and 53.8 ± 1.2 years in the southern sea of Korea-all exceeding the radiological half-life of ¹³⁷Cs (30.17 years). These findings offer quantitative insights that can enhance future predictions of the variability in artificial radionuclide activities, such as ¹³⁷Cs and ²³⁹,²⁴⁰Pu, in Korean seas, where external inputs from surrounding regions play significant roles.
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Lee et al. (2025) studied this question.
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