美国德克萨斯州阿米斯塔德国际水库沉积物中汞的分布

Jesse C. Becker, A. Groeger
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引用次数: 0

摘要

汞(Hg)是一种被广泛研究的水生生态系统污染物,但对其在大型水库,特别是亚热带和热带地区水库中的分布情况知之甚少。确定汞在水生生态系统中的空间分布对于了解其如何在系统中循环具有重要意义。大多数涉及空间成分的汞调查都是在更大的尺度上进行的(例如GILMOUR等人1998年,DAVIS等人2008年)或在北方和温带地区进行的(例如GoRSKI等人2003年)。阿米斯塔德国际水库是一个大型亚热带水库,位于美国德克萨斯州和墨西哥厄阿韦拉之间的边界(北纬29°27;101°03'W),位于格兰德河/Río Bravo流域。在保护水平(340.5米a.s.l),覆盖约263公里。水库是低营养的,具有高碱度和pH值,低溶解有机碳(DOe);IBWe 1997, TeEQ 2004)和低湿地面积(作者,论文。observ)。这些特征通常与生物群中汞含量升高无关。VANMETRE等人(1997)使用2个沉积物岩心发现,随着时间的推移,水库沉积物中总汞含量较低,但在不断增加(地表40-50 ppb),并将这种增加的大部分与大气来源联系起来。盆地中唯一的天然汞源位于大弯地区上游约250公里处。这个地区被称为Terlingua矿区,在1973年矿山关闭之前是美国第三大汞矿区(GRAY et al. 2006)。我们对沉积物中总汞的变化进行了初步描述,并对该系统中总汞的运动进行了一些潜在的影响。迄今为止的结果表明,格兰德河(RG)支流的负荷较高,而魔鬼河(DR)支流的条件可能有利于无机汞向有机甲基汞(meHg)的转化。对鱼类组织的分析表明,甲基汞在该系统的大型运动鱼类中积累。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Distribution of mercury in the sediments of Amistad International Reservoir, Texas, USA
Mercury (Hg) is a widely studied pollutant of great concern in aquatic ecosystems, yet we know little about its distribution in large reservoirs, especially those in subtropical and tropical regions. Determining the spatial distribution of Hg in aquatic ecosystems is important for understanding how it cycles through systems. Most of the Hg investigations involving a spatial component have been done on larger scales (e.g. GILMOUR et al. 1998, DAVIS et al. 2008) or in boreal and temperate regions (e.g. GoRSKI et al. 2003). Amistad International Reservoir is a large subtropical reservoir located on the border between Texas, United States, and eoahuila, Mexico (29°27'N; 101 °03'W), in the Rio Grande/Río Bravo drainage basin. At conservation level (340.5 m a.s.l.) it covers approximately 263 km• The reservoir is oligotrophic with high alkalinity and pH, low dissolved organic carbon (DOe; IBWe 1997, TeEQ 2004), and low wetland area (authors, pers. observ.). These characteristics are not usually linked to elevated Hg levels in biota. VANMETRE et al. (1997) found low but increasing levels of total Hg over time in the sediments o f the reservoir (40-50 ppb at the surface) using 2 sediment cores and linked much of this increase to atmospheric sources. The only native sources of Hg in the basin are approximately 250 km upstream in the Big Bend region. This area, known as the Terlingua Mining District, was the third largest Hg mining area in the United States until the mines were closed in 1973 (GRAY et al. 2006). We present a preliminary description of the variation in sediment total Hg and some potential influences on the movement o f this H g through the system. Results to date suggest higher loading to the Rio Grande (RG) arm of the reservoir, while the Devils River (DR) arm has conditions that may facilitate the transformation of inorganic Hg into organic methyl mercury (meHg). Analysis offish tissue indicates that meHg i s accumulating in the large sport fish o f the system.
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