Titlebook: Advances in Research in Karst Media; Bartolomé Andreo,Francisco Carrasco,James W. LaMor Book 2010 Springer-Verlag Berlin Heidelberg 2010 E

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Resources Assessment of a Small Karstic Mediterranean Aquifer (South-Eastern, Spain)erranean semiarid environments, are sensitive to climatic and anthropogenic changes. Many of them have been severely depleted due to intensive pumping. Drawdowns in the Ventos aquifer amount to approximately 80 m over the last three decades. Adequate knowledge of groundwater resources is necessary f

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Sensitivity Analysis of APLIS Method to Compute Spatial Variability of Karst Aquifers Recharge at thfluenced the recharge are taken into consideration, with a special emphasis on carbonate aquifers. The methodology is applied to carbonated aquifers of the tropical mountains at the National Park of Viñales. As the method has been developed from Mediterranean conditions, some modifications were requ

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First Outcomes from New Approach in Assessing Recharge of Highly Karstified Terrains – Cases Exampleegetation, soil, geology etc. Selection of adequate method for assessing recharge in karst often represents matter of dispute. Multi-parametermethods using GIS tools have been recently successfully developed and applied in karstic terrains of Spain (Andreo et al. 2008) and Lebanon (Shaban et al. 200

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Climate Change Effects on Aquifer Recharge in a Glacierised Karst Aquifer System, Tsanfleuron-Sanetswill disappear within 50 years. The Tsanfleuron-Sanetsch area in the Swiss Alps is an ideal site to study glacier-aquifer interactions; it consists of a vanishing glacier overlying a karst aquifer drained by a spring (Glarey) used for drinking water supply. Between the glacier and the moraine from 1

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Flow Potential Between Stacked Karst Aquifers in Central Texas, USAe overlain by the karstic Upper Trinity and Edwards Aquifers, the degree of karstification is not known, but groundwater in certain units of the Middle Trinity Aquifer is chemically similar to shallow groundwater in this area. Geochemical, potentiometric, and hydraulic conductivity data suggest that

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Access to Coastal Karst Water Resources Through a Salinity Study During an Exceptional High-Water Evn a high water discharge period recorded during December 2008 at Port-Miou spring. During this one week event, the discharge in the 20 m diameter saturated conduit had probably been in the range of 50 to 100 m./s. In spite of this huge spring water discharge, the salinity remained persistently above

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