Page 4: Research news on groundwater and surface-water interaction

Groundwater and surface-water interaction refers to the bidirectional exchange of water, solutes, heat, and sometimes contaminants between aquifers and surface-water bodies such as rivers, lakes, wetlands, and estuaries. This interaction is governed by hydraulic gradients, permeability contrasts, geological heterogeneities, and temporal variability in recharge and evapotranspiration. It encompasses processes such as baseflow discharge, bank storage, hyporheic exchange, and infiltration from surface water to aquifers, which together control streamflow regimes, water quality, redox conditions, and ecological habitat. Quantifying these exchanges is critical in hydrologic modeling, water-budget analysis, contaminant transport studies, and integrated water-resources management under changing climatic and anthropogenic stresses.

Groundwater, a missing link in coastal carbon storage

As global efforts intensify around restoring coastal wetlands to curb climate change, a new JCU-led study published in Reviews of Geophysics is the first to link wetland restoration and carbon cycling with groundwater dynamics, ...

Tracing mountain water to its hidden sources

In mountain regions like the Rockies, headwater streams make up more than 70% of the river network and support the downstream waterways and communities. These headwaters are also home to many forms of aquatic life. While ...

page 4 from 6