Saline Water Intrusion in Coastal Aquifers: Mechanics and Remediation Strategies
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In coastal unconfined aquifers, fresh groundwater floats on denser seawater due to a slight density difference. The interface between fresh and saltwater is governed hydrostatically by the Ghyben-Herzberg Relation, which indicates that for every unit meter of fresh water table elevation above mean sea level, the freshwater-seawater interface extends approximately forty units below sea level:
z = 40 * h
When excessive pumping lowers the freshwater hydraulic head near coastlines, the saline interface moves upward and inland (saltwater intrusion), contaminating coastal production wells and rendering groundwater unfit for irrigation or drinking.
Along vulnerable coastal stretches in India—such as parts of Saurashtra in Gujarat, coastal Tamil Nadu, and Kerala—intense groundwater drafting has triggered severe saltwater intrusion.
Contemporary hydrogeological remediation strategies involve constructing subsurface dikes (underground barriers), artificial recharge injection wells using treated wastewater, and freshwater recharge basins along river mouths. Combined with real-time electrical resistivity tomography (ERT) and continuous borehole salinity logging, engineers can monitor and control the saltwater wedge dynamically.
Note: This technical content was curated and structured with AI assistance to support technical education.
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