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美国东部两个流域溶解甲基汞的空间和季节性变化。

Spatial and seasonal variability of dissolved methylmercury in two stream basins in the eastern United States.

机构信息

US Geological Survey, 720 Gracern Road, Suite 129, Columbia, South Carolina 29210-7651, United States.

出版信息

Environ Sci Technol. 2011 Mar 15;45(6):2048-55. doi: 10.1021/es103923j. Epub 2011 Feb 22.

DOI:10.1021/es103923j
PMID:21341694
Abstract

We assessed methylmercury (MeHg) concentrations across multiple ecological scales in the Edisto (South Carolina) and Upper Hudson (New York) River basins. Out-of-channel wetland/floodplain environments were primary sources of filtered MeHg (F-MeHg) to the stream habitat in both systems. Shallow, open-water areas in both basins exhibited low F-MeHg concentrations and decreasing F-MeHg mass flux. Downstream increases in out-of-channel wetlands/floodplains and the absence of impoundments result in high MeHg throughout the Edisto. Despite substantial wetlands coverage and elevated F-MeHg concentrations at the headwater margins, numerous impoundments on primary stream channels favor spatial variability and lower F-MeHg concentrations in the Upper Hudson. The results indicated that, even in geographically, climatically, and ecologically diverse streams, production in wetland/floodplain areas, hydrologic transport to the stream aquatic environment, and conservative/nonconservative attenuation processes in open water areas are fundamental controls on dissolved MeHg concentrations and, by extension, MeHg availability for potential biotic uptake.

摘要

我们评估了在南卡罗来纳州的埃迪斯托(Edisto)和纽约州的上哈得逊(Upper Hudson)流域的多个生态尺度上的甲基汞(MeHg)浓度。在这两个系统中,河道外湿地/洪泛区环境是溪流生境中过滤甲基汞(F-MeHg)的主要来源。两个流域的浅水开阔水区的 F-MeHg 浓度较低,F-MeHg 质量通量呈下降趋势。在埃迪斯托,由于河道外湿地/洪泛区的增加和没有水坝,导致甲基汞浓度升高。尽管在上游边缘地区湿地面积大,F-MeHg 浓度高,但主要河道上的大量水坝有利于空间变异性,并降低了上哈得逊的 F-MeHg 浓度。结果表明,即使在地理、气候和生态条件多样的溪流中,湿地/洪泛区的生产、向溪流水生环境的水文输送以及开阔水区的保守/非保守衰减过程,都是控制溶解态甲基汞浓度的基本因素,进而也是控制甲基汞对潜在生物吸收的可用性的基本因素。

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