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Radionuclide sorption dynamics in the Rhone River: Experimental and modelling approach
Léonore Flipo1, Frédéric Coppin1, L Garcia-Sanchez1
1Institut de Radioprotection et de Sûreté Nucléaire (IRSN), PSE-ENV/STAAR/LRTA, PSE-ENV/SPDR/LT2S, Saint-Paul-lez-Durance, F-13115, France.
Kinetic models offer more accurate radionuclide transfer predictions in rivers than equilibrium models, especially when environmental conditions change. These models better capture the complex solid/liquid fractionation of contaminants like cesium and cobalt.
Area of Science:
- Environmental Science
- Radiochemistry
- Environmental Modeling
Background:
- Radionuclide transfer in rivers is often modeled using the equilibrium distribution coefficient (Kd), assuming instantaneous and reversible solid/liquid fractionation.
- This equilibrium assumption may underestimate dissolved fractions and fail to account for environmental changes affecting radionuclide partitioning.
- Slower adsorption kinetics and environmental shifts (e.g., confluences, dams) necessitate more dynamic modeling approaches.
Purpose of the Study:
- To evaluate the accuracy of kinetic fractionation models compared to the traditional equilibrium (Kd) approach for radionuclide transfer in rivers.
- To assess the ability of different models (Kd, one-kinetic, two-kinetic) to predict radionuclide behavior under changing environmental conditions.
Main Methods:
- Experimental determination of solid/liquid fractionation kinetics for 137Cs, 60Co, 54Mn, and 110mAg using Rhone River suspended particulate matter over 2 months.
- Simulated environmental condition changes via suspension dilutions after varying adsorption periods (1h to 31 days).
- Fitting experimental data to equilibrium (Kd) and kinetic (EK, KK) models and evaluating predictive capacity for dilution scenarios.
Main Results:
- Radionuclide adsorption kinetics stabilized only after several days to two weeks, contradicting the instantaneous assumption of the Kd model.
- Dilution induced initial radionuclide release followed by unexpected re-adsorption, highlighting non-equilibrium dynamics.
- Kinetic models (EK, KK) predicted variations in solid/liquid activity ratios with time and environmental changes, unlike the constant Kd model.
Conclusions:
- Kinetic models provide more realistic estimations of radionuclide solid/liquid fractionation in rivers than the equilibrium Kd approach.
- Models incorporating kinetics are essential for accurately predicting radionuclide transfer dynamics, especially when facing environmental perturbations.
- One-step sorption kinetic models showed limitations in reproducing complex adsorption behaviors observed after dilution events.
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