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Transport simulation with stochastic aperture for a single fracture – comparison with a laboratory experiment
Ist Teil von
Advances in water resources, 2002, Vol.25 (1), p.19-32
Ort / Verlag
Oxford: Elsevier Ltd
Erscheinungsjahr
2002
Quelle
Access via ScienceDirect (Elsevier)
Beschreibungen/Notizen
In order to investigate the migration behaviour of dissolved solutes in a fractured sedimentary host rock two laboratory experiments using pyranine as tracer were performed in a fractured sandstone block. During a first attempt, the experimental breakthrough curves were used to calibrate a three-dimensional numerical model based on the parallel plate approach. In a second approach, the natural roughness of the fracture surface was added to the model by assigning spatially variable apertures to the fracture elements. The experimental results indicate that the matrix diffusion has a decisive influence on the transport process, acting as a retardation term. The numerical investigation shows that solute migration is controlled by the mean aperture of the single fracture. If the variance of the fracture aperture, however, becomes too large the fracture flow becomes increasingly affected by channelling processes.