Department of Environment & Energy, Sejong University Seoul, 143-747, Republic of Korea.
Sci Total Environ. 2011 Sep 1;409(19):3801-11. doi: 10.1016/j.scitotenv.2011.05.055. Epub 2011 Jul 2.
Concentrations of total gaseous mercury (TGM) were measured continuously at four urban residential locations (G (Guro-gu); N (Nowon-gu); S (Songpa-gu); and Y (Yongsan-gu)) in Seoul, Korea from 2004 to 2009. The mean concentrations of Hg at these sites were found on the order of N (3.98±1.68 ng m(-3)), S (3.87±1.56 ng m(-3)), G (3.80±1.60 ng m(-3)), and Y (3.36±1.55 ng m(-3)). Evidence indicates that the spatial distribution of Hg should be affected by the combined effects of both local anthropogenic (incineration facilities and thermal power plants) and natural (soil) emission sources in association with the meteorological parameters. Inspection of the Hg temporal patterns indicates the co-existence of contrasting seasonal patterns between the central site Y (winter dominance) and all other outbound sites near city borders (summer dominance). The long-term trend of Hg, if examined by combining our previous studies and the present one, shows that Hg levels in this urban area declined gradually across decadal periods despite slight variabilities in spatial scale: (1) above 10 ng m(-3) in the late 1980s, (2) ~5 ng m(-3) in the late 1990s, and (3) ~3 ng m(-3) toward the late 2000s. The results of the principal component analysis along with observed differences in seasonal patterns (between study sites) suggest that Hg distributions between different urban sites are greatly distinguishable with strong source signatures at each individual site.
2004 年至 2009 年,在韩国首尔的四个城市居民区(Guro-gu(G 区);Nowon-gu(N 区);Songpa-gu(S 区)和 Yongsan-gu(Y 区))连续测量了总气态汞(TGM)的浓度。这些地点的 Hg 平均浓度分别为 N(3.98±1.68ng m(-3))、S(3.87±1.56ng m(-3))、G(3.80±1.60ng m(-3)) 和 Y(3.36±1.55ng m(-3))。有证据表明,Hg 的空间分布应受到当地人为(焚烧设施和火力发电厂)和自然(土壤)排放源与气象参数共同作用的影响。对 Hg 时间模式的检查表明,市中心 Y 站点(冬季主导)和城市边界附近的所有其他出站站点之间存在相反的季节性模式(夏季主导)。如果将我们之前的研究和当前的研究结合起来检查 Hg 的长期趋势,表明尽管在空间尺度上存在细微的变化,但该城市地区的 Hg 水平在过去几十年中逐渐下降:(1)在 20 世纪 80 年代末超过 10ng m(-3),(2)在 20 世纪 90 年代末5ng m(-3),(3)在 2000 年代末3ng m(-3)。主成分分析的结果以及观察到的季节模式差异(在研究站点之间)表明,不同城市站点之间的 Hg 分布差异很大,每个站点都有明显的源特征。