Groundwater and surface water are intimately linked, being part of the same overall hydrological cycle. Aquifers discharge to surface water bodies, and can be recharged by them, depending on local conditions. However, while river systems are naturally dominated by flow most aquifers are dominated by storage, and this has some fundamental implications: (a) aquifers have a large capacity to buffer surface water variability and drought cycles; (b) the...
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ПОДРОБНАЯ ИНФОРМАЦИЯ
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2006/01/01
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Краткие сведения
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44293
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1
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1
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2010/10/29
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Disclosed
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El agua subterranea en la planificacion hidrica nacional y de cuencas : promover una estrategia integral
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aquifer
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