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Trace Metals in Upland Headwater Lakes in Ireland

机译:爱尔兰高地源头湖泊中的痕量金属

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Trace elements (n = 23) in Irish headwater lakes (n=126) were investigated to determine their ambient concentrations, fractionation (total, dissolved, and non-labile), and geochemical controls. Lakes were generally located in remote upland, acid-sensitive regions along the coastal margins of the country. Total trace metal concentrations were low, within the range of natural pristine surface waters; however, some lakes (~20%) had inorganic labile aluminum and manganese at levels potentially harmful to aquatic organisms. Redundancy analysis indicated that geochemical weathering was the dominant controlling factor for total metals, compared with acidity for dissolved metals. In addition, many metals were positively correlated with dissolved organic carbon indicating their affinity (or complexation) with humic substances (e.g., aluminum, iron, mercury, lead). However, a number of trace metals (e.g., aluminum, mercury, zinc) were correlated with anthropogenic acidic deposition (i.e., non-marine sulfate), suggesting atmospheric sources or elevated leaching owing to acidic deposition. As transboundary air pollution continues to decline, significant changes in the cycling of trace metals is anticipated.
机译:对爱尔兰源头湖泊(n = 126)中的痕量元素(n = 23)进行了研究,以确定它们的环境浓度,分馏(总,溶解和不稳定)和地球化学控制。湖泊通常位于该国沿海边缘的偏远山区,对酸敏感。在天然原始地表水范围内,痕量金属的总浓度较低。但是,一些湖泊(约20%)的无机不稳定的铝和锰含量可能对水生生物有害。冗余分析表明,与溶解金属的酸度相比,地球化学风化是总金属的主要控制因素。另外,许多金属与溶解的有机碳呈正相关,表明它们与腐殖质(例如铝,铁,汞,铅)的亲和力(或络合)。但是,许多痕量金属(例如铝,汞,锌)与人为的酸性沉积物(即非海洋硫酸盐)相关,表明大气源或由于酸性沉积物而增加的淋洗。随着越境空气污染的持续下降,预计痕量金属的循环将发生重大变化。

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