酸性矿井排水退化水系的定量水化学变化趋势

D. Graebe, J. Wood
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摘要

数百年来,露天煤矿开采一直是阿巴拉契亚地区的主要经济力量。露天煤矿开采产生的径流被称为酸性矿井水(AMD),它渗入淡水溪流并严重退化。酸性矿井水影响河流的生物多样性显著减少,尤其是对污染不耐受的蜉蝣目、翼翅目和毛翅目(EPT)类群。我们研究了四条溪流的水质。两个下游矿山受到AMD的影响,而另外两个作为对照或未受损的站点。使用YSI 9500光度计测量了所有四条河流的水化学成分,包括硫酸盐、铁和镁。使用YSI Quatro计测量每条溪流的pH值。我们发现,在受损的溪流中,硫酸盐和铁的水平升高,而镁的水平在不同的地点有所不同。受损溪流的pH值趋于较低,但仍保持相当碱性(pH值bbb50)。这些数据有助于了解受损溪流的化学性质,以及淡水大型无脊椎动物如何对这些化学参数做出反应。此外,这些数据有助于可能依赖于特定水化学的补救工作。
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Quantifiable Water Chemistry Trends in Streams Degraded by Acid Mine Drainage
Surface coal mining has been a major economic force in the Appalachian region for hundreds of years. Surface coal mining leads to runoff known as acid mine drainage (AMD) which infiltrates and severely degrades freshwater streams. Acid mine drainage impacted streams often see a marked decrease in biodiversity especially Ephemeroptera, Plecoptera, and Trichoptera (EPT taxa) which are intolerant to pollution. We researched the water quality in four streams. Two downstream mines were impacted by AMD while the other two served as control or unimpaired sites. Water chemistry of all four streams was measured including sulfate, iron, and magnesium using a YSI 9500 photometer. The pH of each stream was measured using a YSI Quatro meter. We found elevated levels of sulfate and iron in the impaired streams while magnesium levels varied across sites. The pH tended to be lower in the impaired streams but remained fairly alkaline ( pH > 5). These data are useful for understanding the chemistry of impaired streams and how freshwater macroinvertebrates may respond to these chemical parameters. Additionally these data aid in remediation efforts which may be dependent on specific water chemistry.  
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