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Geographically Isolated Wetlands (GIWs) occur along gradients of hydrologic and ecological connectivity and isolation, even within wetland types (e.g., forested, emergent marshes) and functional classes (e.g., ephemeral systems, permanent systems, etc.). Within a given watershed, the relative positions of wetlands and open-waters along these gradients influence the type and magnitude of their chemical, physical, and biological effects on downgradient waters. In addition, the ways in which GIWs connect to the broader hydrological landscape, and the effects of such connectivity on downgradient waters, depends largely upon climate, geology, and relief, the heterogeneity of which expands with increasing scale. Developing...
This project investigates the spatial and temporal variability of ground-water surface-water exchange in response to changes in the geometry and hydrogeologic properties of this interface that are driven by episodic and sustained fluvial and hydrologic events. Episodic events are common and occur across a broad range of physical and climatic settings and are rarely accounted for in scientific investigations or resource management. Linkages between a dynamic sediment-water interface and the resulting fluxes between ground water and surface water need to be understood, quantified, and modeled to determine their influence on the quantity and quality of our Nation’s water resources as well as the ecological changes...