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Suspended Particle–Water Interactions Increase Dissolved <sup>137</sup>Cs Activities in the Nearshore Seawater during Typhoon Hagibis
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Citations
40
References
2020
Year
Distributions of <sup>137</sup>Cs in dissolved and particulate phases of the downstream reaches of seven rivers and adjacent nearshore and offshore waters as far as ∼60 km south of the Fukushima Dai-ichi nuclear power plant (FDNPP) were studied during the high-river-flow period (June-September 2019) and during the period of October 2019 after typhoon Hagibis. Dissolved <sup>137</sup>Cs activities in nearshore water were higher than those in rivers and offshore waters, and this distribution was more intensified after the typhoon, indicating the desorption of <sup>137</sup>Cs from riverine suspended particles in addition to the ongoing release of contaminated water from the FDNPP and re-entry of radiocesium via submarine groundwater discharge. This scenario is also supported by the reduction of distribution coefficient (<i>K</i><sub>d</sub>) from a geometric mean value of 5.5 × 10<sup>5</sup> L/kg in rivers to 9.8 × 10<sup>4</sup> L/kg in nearshore water. The occupation of desorbed <sup>137</sup>Cs to the dissolved activity of this nuclide in nearshore water was estimated to be 0.7%-20% (median: 9.7%) during the high-river-flow period, increasing to 1.4%-66% (32.3%) after the typhoon, suggesting that the desorption during the flood period such as typhoons further contributes to the increase in dissolved <sup>137</sup>Cs levels in nearshore water.
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