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Titlebook: Overexploitation and Contamination of Shared Groundwater Resources; Management, (Bio)Tec Christophe J. G. Darnault Conference proceedings 2

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Transboundary Aquifers in International Law: Towards an Evolutionwas very scarce and almost non-existent, the situation is now showing signs of change. States sharing an aquifer are seeking to establish cooperation mechanisms over their common resource, and are introducing the consideration of a legal component in projects on transboundary aquifers. In June 2006,
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Quantitative Integration of Hydrogeophysical and Hydrological Data: Geostatistical ApproachesGiven the differing sensitivities of various geophysical techniques to hydrologically relevant parameters and their inherent trade-off between resolution and range as well as the inherently site-specific nature of petrophysical parameter relations, the fundamental usefulness of multi-method surveys
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Hydrogeological Settings in Dobrudja Area and Groundwater Monitoring Networks in Transboundary Aquifof the integrated management of transboundary groundwater between Bulgaria and Romania. The physicochemical characteristics of the Upper Jurassic—Valanginian aquifer (Deep Aquifer) and the Sarmatian aquifer (Upper Aquifer)— are reviewed in details. The groundwater monitoring network developed in the
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Coupled Surface/Subsurface Flow Systems: Numerical Modelingifers as well as open water bodies. First, basic concepts on partially saturated flow systems are presented (mostly without equations). A brief review of a fully 3D modeling approach, involving the concept of a variably saturated macroporous medium, is given. The rest of the chapter focuses on a 2D
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Quantitative Stochastic Hydrogeology: The Heterogeneous Environmentn points: the quantitative representation and generation of heterogeneous geologic media (continuous or discontinuous) in a statistical framework, and the appropriate governing equations to model groundwater flow in such media. The growing interest in “.” is due to the fact that complex spatial patt
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Karst Aquifers: Hydrogeology and Exploitationst water resources. In the Mediterranean and Southeast Asia, karst aquifers are the primary water resources. Karst terrains results from karstification, a phenomenon of dissolution of carbonate rocks under the action of water followed by physicochemical processes. Karst processes use the original di
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