Characterisation of HTO diffusion properties by an in situ tracer experiment in Opalinus clay at Mont Terri.
A long-term single borehole diffusion experiment using tritiated water as tracer was carried out in Opalinus clay, an argillaceous rock formation that is accessible at the Mont Terri Underground Research Laboratory, situated in the Swiss Jura. The tracer was diluted in reconstituted formation water and introduced into a packed-off section of a borehole located in saturated rock. Pressure in this interval was maintained equal to the pore pressure of the surrounding rock in order to prevent any hydraulic gradient around the borehole and to avoid advective transport processes. The evolution of the tracer concentration in the injection system was monitored over time. After 1 year of diffusion, the claystone surrounding the interval was retrieved by overcoring the whole borehole and packer system, and by an adjacent oblique borehole. Compressed air was used as drilling fluid to reduce rock disturbances. The recovered overcore was sampled along profiles perpendicular to the borehole wall with a view to determining the tracer-concentration profiles in the rock. To avoid further evaporation of tritiated water, subsamples were immediately transferred into polyethylene bottles and disaggregated by adding a known amount of tracer-free water. Fifteen profiles were determined and showed a decreasing tracer concentration with distance into the rock. The pore-water contents were constant along those profiles, confirming that only very little water was lost during overcoring operations. The evolution of tritium-tracer concentration in the injection system over time and in situ profiles were interpreted with a 3-D numerical simulation of the experiment. That allowed for the identification of the transport parameters (orthotropic diffusion tensor and porosity) by minimising the relative quadratic error between the experimental and simulated data. The fitting is good and the results are consistent with data obtained on drill-core samples. The result of tritiated water is discussed regarding (1) the potential effect of mechanical and/or chemical disturbances around the injection borehole and (2) the specific behaviour of tritiated water.
Palut
J-M
JM
ANDRA, Parc de la Croix-Blanche, 1-7 rue Jean-Monnet, 92298 Chatenay-Malabry Cedex, France.
Montarnal
Ph
P
Gautschi
A
A
Tevissen
E
E
Mouche
E
E
D000538:Aluminum Silicates / Q000737:chemistry*; D000077215:Clay; D004058:Diffusion; D004784:Environmental Monitoring; D011850:Radioactive Waste; D013557:Switzerland; D014316:Tritium / Q000032:analysis; D018505:Waste Management
D000538:Aluminum Silicates; D011850:Radioactive Waste; D014316:Tritium; D000077215:Clay