Colloid-Facilitated Transport of 137Cs in Fracture-Fill Material. Experiments and Modeling

Dittrich, Timothy M.¹  Reimus, Paul William¹ 

[1] Los Alamos National Lab. (LANL), Los Alamos, NM (United States)

关键词: Earth Sciences;    cesium;    fracture fill material;    granite;    bentonite;   

DOI  :  10.2172/1225270
RP-ID  :  LA-UR--15-28482
PID  :  OSTI ID: 1225270

美国|英语

来源: SciTech Connect

【 摘 要 】

In this study, we demonstrate how a combination of batch sorption/desorption experiments and column transport experiments were used to effectively parameterize a model describing the colloid-facilitated transport of Cs in the Grimsel granodiorite/FFM system. Cs partition coefficient estimates onto both the colloids and the stationary media obtained from the batch experiments were used as initial estimates of partition coefficients in the column experiments, and then the column experiment results were used to obtain refined estimates of the number of different sorption sites and the adsorption and desorption rate constants of the sites. The desorption portion of the column breakthrough curves highlighted the importance of accounting for adsorption-desorption hysteresis (or a very nonlinear adsorption isotherm) of the Cs on the FFM in the model, and this portion of the breakthrough curves also dictated that there be at least two different types of sorption sites on the FFM. In the end, the two-site model parameters estimated from the column experiments provided excellent matches to the batch adsorption/desorption data, which provided a measure of assurance in the validity of the model.