Sediment processes and mercury transport in a frozen freshwater fluvial lake (Lake St. Louis, QC, Canada)
2009
Canário, João | Poissant, Laurier | O'Driscoll, Nelson | Vale, Carlos | Pilote, Martin | Lean, D. R. S. (David R. S)
An open-bottom and a closed-bottom mesocosm were developed to investigate the release of mercury from sediments to the water column in a frozen freshwater lake. The mesoscosms were deployed in a hole in the ice and particulate mercury (HgP) and total dissolved mercury (TDHg) were measured in sediments and in water column vertical profiles. In addition, dissolved gaseous mercury (DGM) in water and mercury water/airflux were quantified. Concentrations of TDHg, DGM, and mercury flux were all higher in the open-bottom mesocosm than in the closed-bottom mesocosm. In this paper we focus on the molecular diffusion of mercury from the sediment in comparison with the TDHg accumulation in the water column. We conclude that the molecular diffusion and sediment resuspension play a minor role in mercury release from sediments suggesting that solute release during ebullition is an important transport process for mercury in the lake. In a frozen lake Hg is released from contaminated sediments mainly due to gas ebullition and molecular diffusion plays a minor role.
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