In the Karst, the drainage of the stalactites can provide information about the laws that govern percolation. The viability of a percolation simulation with analytic models is studied. From the results obtained in Baradia and Béke Caves (Yugoslavia), it happened to be that the drainage through the unsaturated zone in the Karst was apparently similar to th at shown in the hydrographs of the springs and also amenable to mathematical modelling
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