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Mercury Cycling in an Urbanized Watershed: The Influence of Wind Distribution and Regional Subwatershed Geometry in Central Indiana, USA

机译:城市化流域中的汞循环:风分布和区域分水岭几何对美国中部印第安那州的影响

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The global cycle of mercury (Hg) is reasonably well-understood, as are some of the natural and anthropogenic sources of Hg to the atmosphere. Less well understood are the regional and local characteristics of Hg deposition and subsequent watershed-scale transport, important parameters for assessing human risk to various avenues of Hg exposure. This study employed a two-part strategy for understanding coupled deposition and transport processes in central Indiana (USA), including Indianapolis, a typical large city with multiple coal-fired electric utilities and other Hg emission sources. A spatial analysis of Hg concentrations in surface soils revealed elevated Hg proximal to many of the large emission sources, with a distribution aligned along a southwest-northeast axis corresponding to the mean wind direction in this region. This soil distribution suggests some local depositional impact from local utilities, with wind modification affecting the regional pattern. Post-depositional transport of Hg was assessed using a series of streambank sampling arrays as the White River and various tributaries travelled through the urban core of Indianapolis. Streambank sediments had peak Hg concentrations in the urban core, where several local sources are present and where a number of subwatersheds join the main trunk of the White River, suggesting local emission and/or rapid Hg transport from urban subwatersheds due to their relatively high proportion of impervious surfaces. High Hg values persist in White River sediments into rural areas tens of kilometers south of Indianapolis, raising concerns for anglers collecting fish in this apparently "pristine" environment.
机译:汞(Hg)的全球循环以及大气中汞的一些自然和人为来源都得到了很好的理解。汞沉积的区域和局部特征以及随后的分水岭规模的运输,这是评估人类对各种汞接触途径的风险的重要参数,人们对此知之甚少。这项研究采用两部分策略来了解印第安纳州中部(美国)的耦合沉积和运输过程,包括印第安纳波利斯,印第安纳波利斯是一个典型的大城市,拥有多个燃煤电力公司和其他汞排放源。对表层土壤中汞浓度的空间分析表明,在许多大型排放源附近,汞含量升高,其分布沿西南-东北轴线排列,与该区域的平均风向相对应。这种土壤分布暗示了当地公用事业的一些局部沉积影响,而风的变化影响了区域格局。在怀特河和各种支流穿过印第安纳波利斯市区的过程中,使用一系列的河岸采样阵列对汞的沉积后运输进行了评估。河岸沉积物在城市核心地区有最高的Hg浓度,那里有多个地方水源,许多子集水区汇入了怀特河的主要干线,这表明由于城市子集水区的比例相对较高,导致了本地排放和/或Hg的快速迁移不透水的表面。怀特河的沉积物中高的Hg值持续存在于印第安纳波利斯以南数十公里的农村地区,这引起了钓鱼者在这种看似“原始”的环境中捕捞鱼的担忧。

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