A new timescale dimension for migration experiments in clay: proof of principle for the application of miniaturized clay column experiments (MCCE)

Abstract

Geological clay formations are often considered as a host rock for a future nuclear waste repository. Many studies concerning sorption or desorption experiments with metal ions like radionuclides or other relevant substances (e.g. metal complexing ligands) onto/from geological clay samples are performed with the batch techniques where only small amounts of the homogenized clay is in contact with the appropriate metals diluted in high volumes of aqueous solutions. This unnatural contact of clay with water can lead to high bias or not transferable results for a risk assessment study of a future repository. Diffusion experiments as an alternative and more natural experimental tool have the lack of huge time consuming when the migration of higher valent metal ions is considered. With the herein described new miniaturized clay column setup a linker between the unnatural batch techniques and the time consuming diffusion experiments is installed. The presented miniaturized clay column experiments (MCCE) derived and modified from high performance liquid chromatography can be applied in a lot of geochemical studies. Using MCCE, migration experiments of inert tracers (iodide), natural organic matter as complexing ligands (lactate and salicylate) as well as trivalent metal ions (europium) in compacted clay can be performed within a short time span of a few minutes or hours only in contrast to several months by use of classical diffusion or column methods. As preliminary results, typical migration times through miniaturized clay columns (20 × 3.5 mm, L × ID) of iodide as inert tracer are in the range of 145 min, meanwhile increasing retention times of salicylate from about 390 min in the absence of Eu to migration times in the range of 420–470 min in the presence of different Eu concentration can be observed.