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1. Multi-Scale Surface Water-Groundwater Interaction : Implications for GroundwaterDischarge Patterns
Sammanfattning : Rivers and aquifers are continuously exchanging water, driven by processes that occur on various temporal and spatial scales, ranging from small streambed features to large geological structures. The interaction between these two components occurs in permeable sediments below the stream channel, called the hyporheic zone. LÄS MER
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