文摘
One pathway for release of mercury (Hg) from naturallyenriched sites is emission to the atmosphere. Elemental Hg,when emitted, will enter the global atmospheric pool. Incontrast, if reactive gaseous Hg or Hg2+ (as HgCl2, HgBr2,or HgOH2) is formed, it will most likely be depositedlocally. This study focused on the measurement of elementalHg flux and reactive gaseous Hg concentrations at theSulphur Bank Superfund Site, an area of natural Hg enrichmentwith anthropogenic disturbance and ongoing geothermalactivity. Mean Hg emissions ranged from 14 to 11000 ng m-2h-1, with the highest emissions from anthropogenicallydisturbed materials. Reactive gaseous Hg concentrationswere the highest ever reported for a natural setting (0.3-76 ng m-3). Measured Hg fluxes were used within aGeographic Information System to estimate mercury releasesto the atmosphere from the site. Results indicated ~17kg of Hg y-1 of is emitted to the atmosphere from the 3.8km2 area, with half from mine waste, ore, and tailingpiles and half from relatively undisturbed naturally enrichedsubstrate.