Abstract
Chemical analyses have been carried out in the Foussoubie karstic system (France) to understand the origin and the circulation of its water flow. These analyses were made during two different time scales, a whole hydrological cycle, and a flood. The evolution of the chemical composition of the water and particularly the bicarbonate/calcium ratio permit the identification of the kind of infiltration which contributes to the subterranean flow. A qualitative model has been set up to describe the degree of the contribution of infiltration to subterranean discharge.
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