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capacity of water clarifi cation unit to treat. In order to manage this risk,
the spring and a network of 24 piezometers distributed over the entire
watershed are regularly monitored (PĂ©rissol, 2004). The drainage basin,
the limits of which remain poorly defi ned, is estimated to cover between
170 and 200 km 2 .
A similar example exists in Montenegro, in Opacica, near the mouth
of the Kotor, where the karst aquifer can be lowered by 20 m below sea
level, thanks to a favorable geologic environment protecting it from marine
contamination.
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