ROAD SALT IMPACTS GROUNDWATER QUALITY AND RECHARGE IN STORMWATER MANAGEMENT AREAS
We monitored groundwater levels, salinity, and quality beneath a stormwater infiltration basin in Delaware to evaluate salt transport in groundwater and the impacts of road salt on groundwater chemistry. Chloride behaves conservatively, making it an excellent tracer of salt movement in the heterogeneous aquifer beneath the basin. We found that chloride is preferentially transported through higher permeability zones and did not diffuse or disperse through the entire aquifer thickness. Sodium, however, was temporarily retained in shallow soil, leading to a lag time between chloride and sodium movement through the aquifer. Importantly, increasing chloride concentrations were correlated with greater radium concentrations, indicating salty water is mobilizing radium from the aquifer matrix to groundwater.
We have been investigating the dynamics between salt loading, sodium retention in soil, and infiltration rate of the basin surface for multiple years. Reduced infiltration rate leads to a longer residence time of standing water in the basin where salt concentrations may increase as water evaporates prior to infiltration. Our results highlight the importance of considering stormwater impacts on groundwater and the inevitable discharge of salty water to surface water when designing stormwater management infrastructure.