Research news on saltwater intrusion

Saltwater intrusion is the landward migration of saline water into freshwater aquifers, surface waters, or soils driven primarily by hydraulic gradients altered by groundwater pumping, sea-level rise, or reduced recharge. It is governed by variable-density flow and solute transport processes described by coupled groundwater flow and advection–dispersion equations, often producing a transition zone rather than a sharp interface between fresh and saline water. In coastal hydrogeology, saltwater intrusion degrades groundwater quality, alters geochemical equilibria, and constrains sustainable yield, requiring quantitative assessment through monitoring networks, hydrogeologic characterization, and numerical modeling to design mitigation strategies such as pumping optimization, recharge enhancement, or physical barriers.