Submarine Groundwater Discharge as a Source of Mercury in the Bay of Puck, the Southern Baltic Sea

Both groundwater flow and mercury concentrations in pore water and seawater were quantified in the groundwater seeping site of the Bay of Puck, southern Baltic Sea. Total dissolved mercury (HgT(D)) in pore water ranged from 0.51 to 4.90 ng l(−1). Seawater samples were characterized by elevated HgT(D) concentrations, ranging from 4.41 to 6.37 ng l(−1), while HgT(D) concentrations in groundwater samples ranged from 0.51 to 1.15 ng l(−1). High HgT(D) concentrations in pore water of the uppermost sediment layers were attributed to seawater intrusion into the sediment. The relationship between HgT(D) concentrations and salinity of pore water was non-conservative, indicating removal of dissolved mercury upon mixing seawater with groundwater. The mechanism of dissolved mercury removal was further elucidated by examining its relationships with both dissolved organic matter, dissolved manganese (Mn II), and redox potential. The flux of HgT(D) to the Bay of Puck was estimated to be 18.9 ± 6.3 g year(−1). The submarine groundwater discharge-derived mercury load is substantially smaller than atmospheric deposition and riverine discharge to the Bay of Puck. Thus, groundwater is a factor that dilutes the mercury concentrations in pore water and, as a result, dilutes the mercury concentrations in the water column.