RESUMO
Several dry deposition methods for Hg are being developed and tested in our laboratory. These include hig-leaf and multilayer resistance models, micrometeorological methods such as Bowen ratio gradient approaches, Iaboratory controlled plant chambers, and throughfall. We have previously described our initial results using modeling and gradient methods. ThroughfaIl may be used to estimate Hg dry deposition if some simplifying assumptions are met. We describe here the application and initial results of througbfall studies at the Walker Branch Watershed forest, and discuss the influence of certain assumptions on interpretation of the data. Throughfall appears useful in that it can place a lower bound to dry deposition under field conditions. Our preliminary throughfall data indicate net dry deposition rates to a pine canopy which increase significantly from winter to summer (range ~0.1 to 3 ng/m-2/h-1), as previously predicted by our resistance model. Atmospheric data suggest that rainfall washoff of fine aerosol dry deposition at this site is not sufficient to account for all of the Hg in net throughfall. Potential additional sources include dry deposited gas-phase compounds (Hg° or Hg-Il), soilderived coarse aerosols, and oxidation reactions at the leaf surface.