Fluxes of methylmercury to the water column of a drainage lake: The relative importance of internal and external sources

We studied fluxes of methylmercury (MeHg) through a Precambrian Shield lake using a mass balance approach. The primary goal of the study was to determ ine the importance of various sources of MeHg to the water column of the la ke. The relative importance of all sources was: in-lake production >>> infl ow from a brown-water lake with riparian wetlands >>> wet deposition > infl ow from an upstream oligotrophic lake > direct inflow from uplands surround ing the lake. MeHg accumulated in the hypolimnion of Lake 240 when oxygen w as present. Water-column sinks for MeHg included photodegradation of MeHg, which was about 3.5 times greater than the loss of MeHg through outflow. At present, there are few studies available on mass balance fluxes of MeHg in lakes, and this is the first study that includes losses of MeHg by photode gradation. The inclusion of photodegradation in this study results in a cle ar demonstration that in-lake production of MeHg is very important. In drai nage lakes, the relative importance of in-lake production versus inflow of MeHg from wetlands will vary according to the extent of wetlands in the dra inage basin, as well as the volume of precipitation, which produces runoff and transports MeHg from wetlands to downstream lakes.