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Mercury wet deposition is dependent on both the scavenging of divalent reactive gaseous mercury (RGM) and atmospheric particulate mercury (Hg(p)) by precipitation. Estimating the contribution of precipitation scavenging of RGM and Hg(p) is important for better understanding the causes of the regional and seasonal variations in mercury wet deposition. In this study, the contribution of Hg(p) scavenging was estimated on the basis of the scavenging ratios of other trace elements (i. E. , Cd, Cu, Mn, Ni, Pb and V) existing entirely in particulate form. Their wet deposition fluxes and concentrations in air, which were measured concurrently from April 2004 to March 2005 at 10 sites in Japan, were used in this estimation. The monthly wet deposition flux of mercury at each site correlated with the amount of monthly precipitation, whereas the Hg(p) concentrations in air tended to decrease during summer. There was a significant correlation (P<0. 001) among the calculated monthly average scavenging ratios of trace elements, and the values in each month at each site were similar. Therefore, it is assumed the monthly scavenging ratio of Hg(p) is equivalent to the mean value of other trace elements. Using this scavenging ratio (W), the wet deposition flux (F) due to Hg(p) scavenging in each month was calculated by F=WKP, where K and P are the Hg(p) concentration and amount of precipitation, respectively. Relatively large fluxes due to Hg(p) scavenging were observed at a highly industrial site and at sites on the Japan Sea coast, which are strongly affected by the local sources and the long-range transport from the Asian continent, respectively. However, on average, at the 10 sites, the contribution of Hg(p) scavenging to the annual mercury deposition flux was 26%, suggesting that mercury wet deposition in Japan is dominated by RGM scavenging. This RGM should originate mainly from the in situ oxidation of Hg0 in the atmosphere. [Copyright &y& Elsevier]

Abstract: The annual wet and dry deposition fluxes of 12 trace elements (i.e., As, Cd, Cr, Cu, Hg, Mn, Mo, Ni, Pb, Sb, Se and V) were measured on the basis of 1 year of observations (December 2003–November 2004) at 10 sites in Japan. Precipitation and dry deposition (gases and particles) samples were collected every half month using an automatic sampler, which is composed of a precipitation sampler and a water surface sampler for dry deposition. The wet deposition fluxes of Hg, Pb and Se exceeded their dry deposition fluxes at most sites. In contrast, the dry deposition fluxes of Cr, Cu, Mn, Mo, Ni and V were significantly higher than their wet deposition fluxes. The annual wet deposition fluxes of trace elements except for Cu, Mo and Ni were correlated with the annual precipitation amount (). In particular, about 70–80% of the variance of the wet deposition fluxes for Hg (), Sb () and V () was explained using the precipitation amount. The wet deposition fluxes of As, Cd, Pb and Se at sites on the Japan Sea coast tended to be higher than those expected from the precipitation amount. This suggests a large contribution of their long-range transport from the Asian continent. On the other hand, the regional variations in the dry deposition fluxes of the trace elements were different from those in the wet deposition fluxes. A markedly higher dry deposition fluxes were observed at sites in industrial and urban areas. The relatively high dry deposition fluxes of Cr, Cu, Mn, Ni and Pb suggest that these elements are mainly from electric steel furnaces near the sites, because they are abundant in furnace emission particles. The results of lead isotope analyses indicate that the lead isotope ratios in the dry deposition samples at industrial and urban sites are different from those at other sites. This implies that lead dry deposition at such sites is dominated by emissions from peculiar sources, although whether those sources are the electric steel furnaces is unknown. [Copyright &y& Elsevier]