Titlebook: Eurokarst 2018, Besançon; Advances in the Hydr Catherine Bertrand,Sophie Denimal,Philippe Renard Conference proceedings 2020 Springer Natur

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Karst and Vegetation: Biodiversity and Geobotany in the Sierra de las Nieves Karst Aquifer (Málaga, .. Vegetation is mainly controlled by the soil development and climatic conditions. In turn, the soil is controlled by lithology, fracturing, weathering and slope. There is also positive of soil and vegetation feedback in the epikarst development. This study focuses on the spatial variability of veg

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Geological Setting of the Païolive Karst (Ardèche, South of France): Consequences on its Genesis and of the karst that affects late Jurassic limestone. Results point to paleo-surface abandonment, river incision and karst formation resulting from a late Miocene and pre-Messinian uplift of the area. The epigene karst does not extend below the present-day base level.

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From Jovan Cvijic to Alain Mangin or How a Karst Landscape Was Transformed into a Complex Karst Hydrf pipes through which man and water could pass. Because it is generally an arid surface landscape, it was seen as a combination of forms resulting essentially from climatic actions. As a groundwater reservoir discharging to often spectacular springs, it was considered as a fractured or fissured aqui

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Use of Chlorophyll-a Monitoring to Determine Karst–River Relationships: A Case Study in the Karstic nts in a karstic aquifer, the water and sanitation department of Dijon Metropole tested a chlorophyll-a probe in addition to pressure and temperature probes. The field tests were performed in karstic Bathonian limestones near a canal, where eutrophication occurs in summer. The study site, called Cru

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Karst–River Interaction, Elaboration of an Indicator of the Karst Hydrological Conditions Applied to parameter in a modeling procedure, a Hydric Indicator of the Karst (HIK) was established from the knowledge acquired on the functioning of the karstic hydrosystem of the Cèze. This indicator makes it possible to identify and qualify if at a specific moment “t” the karst is more able to contribute t

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