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Very little is known of the factors controlling soil-to-plant transfer of radionuclides in tropical environments.
In his studies, he participated in the project of the workshop of Interdisciplinary Study on Environmental Transfer of Radionuclides from the Fukushima Daiichi NPP Accident (ISET-R) to shed light on the environmental transfer of radionuclides and to contribute to the revival of the affected areas in the Fukushima prefecture.
This implies that the release and transfer of radionuclides from the repository into the surface environment are calculated and that the effects in the biosphere are evaluated for an assessment period up to one hundred thousand years according to Swedish regulations.
For decades, transfer of radionuclides from the environment through the food chain to humans has been the major pathway of the exposure to chronic low-dose radiation [ 7].
Taking into account the same mechanism for the transfer of radionuclides from soil to water, we can suppose that the lack of water flow in the case of lakes does not allow for removal of radionuclides coming into the water.
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In addition, the transfers of radionuclides between the liquid and solid phases are described in terms of kinetic transfer coefficients.
Transport factor refers to the transport of radionuclides on transportation arteries and the transfer of these agents to the human population residing in the vicinity of these arteries.
Because of concerns over mining impacts and the efficient transfer of airborne radionuclides through the lichen-caribou-human food chain, radionuclides were analyzed in tissues from 18 barren-ground caribou (Rangifer tarandus groenlandicus).
The temperature rise leads to an increase in the distribution coefficients and to the further transfer of the radionuclides into the solid phase.
In the decade immediately following the closure of the LFBG, substantial transfer of various radionuclides from the buried waste to the overlying soil was observed.
Soil-to-plant transfer of a radionuclide was quantified with its aggregated transfer factors specified for the time periods from deposition until harvest (Taag, m2 kg−1).
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