In this study, the goal is to assess the temporal and spatial variation of Hg isotope ratios by analyzing depths profiles in sediment cores at different distances from a point source, a metal smelting operation. The study site is the typical mining town-- Flin Flon at Manitoba. Three lake cores were selected along the main wind direction (NW-SE) from the smelter: Phantom Lake, 5km; Cleaver Lake, 23km and Mclurg Lake, 73km. All three lake cores had distinct Hg isotopic compositions, which were significantly different among lakes (P<0.0000001). The d202Hg of the Phantom core ranged from -0.67 to -1.48‰, while d202Hg of the furthest Mclurg core varied from -1.44 to -2.71‰. The Cleaver core showed a wider range of d202Hg from -0.79 to 2.48‰. Phantom Lake was dominated by heavier isotopes with higher Hg content. Mclurg Lake served as the Hg background site and was enriched in lighter isotopes. Cleaver Lake had the mixture of two different Hg sources: smelter and background. Mass independent fractionation (∆199Hg and ∆201Hg) was not detected in those sediment cores. Moreover, by applying a binary mixing model, we demonstrated the relative contribution of anthropogenic sources in different samples and also provided evidence of the smelter impact on those sediment cores.
This study provided another example to successfully use Hg isotopic composition to track and quantify Hg pollution sources and ultimately to better understand Hg biogeochemical cycling in the environment.