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- W2793944300 abstract "The intake area of the Fontaine de Vaucluse system is more than 1100 km2 wide, with an average altitude of 870 m. The thickness of the lower cretaceous limestones (1500 m) gives the system a very thick (800 m) unsatura¬ ted zone. Karstification is highly developed on the intake area (four caves are more than 500 m deep) as well as on the lower part (pit of 300 m depth under the spring). The bottom of the shafts of the Plateau does not reach the unsaturated zone of the karst, as their flows have the chemical content of seepage water. The maximum hydraulic gradient from the Plateau to the spring is low , only 0.3 %. Dyings permit the assignment of the Ventoux-Lure range (including its calcareous northern side with a southward dipping) and the Vaucluse Plateau to the intake area. The moisture balance, computed at altitude belts shows that the rainfall increases strongly with altitude : 120 mm below 200 m, 1380 mm over 1800 m. The working of the system, studied by means of discharge and physical and chemical content, is one of a well karstified environment, that reacts with slight inertia upon to rainy periods, and that is made up of important reserves, particularly within the unsaturated zone, that supply long decline and depletion episodes." @default.
- W2793944300 created "2018-03-29" @default.
- W2793944300 creator A5029593848 @default.
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- W2793944300 date "1991-01-01" @default.
- W2793944300 modified "2023-09-26" @default.
- W2793944300 title "Le karst de la fontaine de Vaucluse (Vaucluse, Alpes de Haute-Provence, Drôme)" @default.
- W2793944300 cites W2587974636 @default.
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- W2793944300 doi "https://doi.org/10.3406/karst.1991.2268" @default.
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