Balogh Steven J, Swain Edward B, Nollet Yabing H
Metropolitan Council Environmental Services, St Paul, MN 55106-6724, USA.
Sci Total Environ. 2006 Sep 1;368(1):138-48. doi: 10.1016/j.scitotenv.2005.09.045. Epub 2005 Oct 27.
Previous studies have identified flooded landscapes (e.g., wetlands, impoundments) as sites of elevated methylmercury (MeHg) production. Here we report MeHg and total Hg (THg) concentrations and mass loadings in rivers in Minnesota during major flooding episodes in the summer of 2002. Frequent intense precipitation events throughout the summer resulted in extraordinarily wet conditions in east-central and northwestern Minnesota. Streamflow remained at record-setting high levels in many rivers and streams in these regions for several weeks. We observed high concentrations of MeHg (>1.4 ng/L) accompanied by high MeHg/THg ratios (0.39 to 0.50) in the Roseau River in northwestern Minnesota and in the Elk and Rum Rivers in east-central Minnesota. Very high MeHg mass loadings were observed in the Mississippi River just upstream of Minneapolis on July 17 (51 g MeHg/day) and July 23 (42 g MeHg/day), when MeHg concentrations at this site were 0.89 and 0.99 ng/L, respectively. The elevated MeHg concentrations in the Roseau River were associated with low dissolved oxygen and high dissolved reactive phosphorus concentrations, both of which are characteristic of anoxic waters. These rivers drain landscapes containing varying amounts of wetlands, and some of the MeHg discharged is thought to have been flushed from anoxic wetland soils. In addition, the flooding of vast areas of normally dry land surfaces probably also resulted in increased MeHg production, adding to the quantities of MeHg exported from these watersheds. Changing climate patterns are expected to result in more frequent heavy precipitation and flooding events in Minnesota. Our results suggest that as flooding and wet conditions in this region increase, the production of MeHg and its export from terrestrial areas to surface waters will increase also.
以往的研究已确定被洪水淹没的地貌(如湿地、蓄水池)是甲基汞(MeHg)产量升高的区域。在此,我们报告了2002年夏季明尼苏达州河流在主要洪水事件期间的甲基汞和总汞(THg)浓度及质量负荷。整个夏季频繁的强降水事件导致明尼苏达州中东部和西北部出现异常湿润的状况。在这些地区的许多河流和溪流中,径流持续数周保持创纪录的高水平。我们在明尼苏达州西北部的罗索河以及中东部的麋鹿河和拉姆河中观察到高浓度的甲基汞(>1.4 ng/L),同时伴有高甲基汞/总汞比率(0.39至0.50)。7月17日(51克甲基汞/天)和7月23日(42克甲基汞/天),在明尼阿波利斯上游的密西西比河中观察到非常高的甲基汞质量负荷,此时该地点的甲基汞浓度分别为0.89和0.99 ng/L。罗索河中甲基汞浓度升高与低溶解氧和高溶解活性磷浓度有关,这两者都是缺氧水体的特征。这些河流流经包含不同数量湿地的地貌,部分排放的甲基汞被认为是从缺氧的湿地土壤中冲刷出来的。此外,大片通常干燥的陆地表面被洪水淹没可能也导致甲基汞产量增加,从而增加了从这些流域输出的甲基汞量。预计气候变化模式将导致明尼苏达州更频繁地出现强降水和洪水事件。我们的结果表明,随着该地区洪水和湿润状况增加,甲基汞的产量及其从陆地区域向地表水的输出也将增加。