Multitracer test approach to characterize reactive transport in karst aquifers.
A method to estimate reactive transport parameters as well as geometric conduit parameters from a multitracer test in a karst aquifer is provided. For this purpose, a calibration strategy was developed applying the two-region nonequilibrium model CXTFIT. The ambiguity of the model calibration was reduced by first calibrating the model with respect to conservative tracer breakthrough and later transferring conservative transport parameters to the reactive model calibration. The reactive transport parameters were only allowed to be within a defined sensible range to get reasonable calibration values. This calibration strategy was applied to breakthrough curves obtained from a large-scale multitracer test, which was performed in a karst aquifer of the Swabian Alb, Germany. The multitracer test was conducted by the simultaneous injection of uranine, sulforhodamine G, and tinopal CBS-X. The model succeeds to represent the tracer breakthrough curves (TBCs) of uranine and sulforhodamine G and verifies that tracer-rock interactions preferably occur in the immobile fluid region, although the fraction of this region amounts to only 3.5% of the total water. However, the model failed to account for the long tailing observed in the TBC of tinopal CBS-X. Sensitivity analyses reveal that model results for the conservative tracer transport are most sensitive to average velocity and volume fraction of the mobile fluid region, while dispersion and mass transfer coefficients are least influential. Consequently, reactive tracer calibration allows the determination of sorption sites in the mobile and immobile fluid region at small retardation coefficients.
Geyer
Tobias
T
Geoscientific Centre, University of Göttingen, Germany. tgeyer@gwdg.de
Birk
Steffen
S
Licha
Tobias
T
Liedl
Rudolf
R
Sauter
Martin
M
D002138:Calibration; D005456:Fluorescent Dyes / Q000032:analysis / Q000737:chemistry; D005618:Fresh Water / Q000032:analysis*; D005858:Germany; D008962:Models, Theoretical; D014872:Water Movements; D014881:Water Supply / Q000032:analysis*
D005456:Fluorescent Dyes