Shifts of radiocesium vertical profiles in sediments and their modelling in Japanese lakes

- Influences of the 2011 Fukushima nuclear accident on lake sediments were traced.
- Shifts of radiocesium vertical profiles in sediments were compared in five lakes.
- Rapid penetration of radiocesium to a certain depth was observed in some lakes.
- A one-dimensional differential sediment model successfully described the shifts.
- Wind-induced stress and sediment porosity are the key parameters for the submodels.

Vertical profiles of radiocesium concentrations were measured in sediment cores collected at various times after the 2011 Fukushima nuclear accident in five Japanese lakes (Hinuma, Kasumigaura, Kitaura, Onogawa and Sohara) with different morphological and trophic characteristics in order to investigate the sedimentation-diffusion processes. In lakes where sediments had high porosities and experienced considerable wave action due to shallowness, we observed rapid penetration of radiocesium to a certain depth just after the accident, followed by downward movement of the peak depths. In contrast, gradual downward transfers of distinct peaks were found in other types of lakes. A one-dimensional differential sediment model with water-sediments interaction processes was constructed to describe the vertical shift of radiocesium profiles. Our proposed submodels relating to the length scales of the mixing using wind-induced stress and porosity of sediments were constructed based on one measurement of the vertical distribution of radiocesium in three lakes (Hinuma, Kasumigaura and Sohara). This model was then validated using samples from those lakes in different years, as well as from two other lakes. Good agreement was obtained. We discuss our findings, the limits of model application, and future research targets.

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