Abstract
Because of the small radius of investigation of hydrogeological standard testing methods, the characterization of karst aquifers is still a challenge. The development of a karst conduit system introduces an element of large contrast in hydraulic conductivity in the hydraulic parameter field of a karst aquifer. It leads to complex flow patterns and transport phenomena that differ significantly from those observed in porous and fissured media. While on a local, i.e., borehole scale, the fissured matrix of karst aquifers can be regarded as a continuum, on a regional, i.e., catchment scale, the drainage of the aquifer system is controlled by the conduit system, which may have a highly anisotropic geometry. Therefore, characterization of karst aquifers requires a differentiated approach by the combination of various hydrogeological field methods or the application of large-scale tests, which cover the scale of dominant aquifer heterogeneities. Existing numerical modeling approaches can be applied for integral data interpretation on catchment scale.
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This work was funded by the Deutsche Forschungsgemeinschaft (DFG; German Research Foundation) under grants no. GE 2173/2-2 and SA 501/24-1.
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Geyer, T., Birk, S., Reimann, T. et al. Differentiated characterization of karst aquifers: some contributions. Carbonates Evaporites 28, 41–46 (2013). https://doi.org/10.1007/s13146-013-0150-9
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DOI: https://doi.org/10.1007/s13146-013-0150-9