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Heavy Metal Concentrations in the Groundwater of the Barcellona-Milazzo Plain (Italy): Contributions from Geogenic and Anthropogenic Sources

机译:巴切罗纳-米拉佐平原(意大利)地下水中的重金属含量:来自成因和人为来源的贡献

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摘要

We collected and analysed 58 samples of groundwater from wells in the Barcellona-Milazzo Plain, one of the most important coastal aquifers of Sicily (Italy), to determine major, minor, and trace element concentrations. In this area, geogenic and anthropogenic sources of heavy metals and other pollutants co-act, making the individuation of the main pollution sources difficult. Our work was aimed at the application of geostatistical criteria for discriminating between these pollution sources. We used probability plots for separating anomalous values from background concentrations, which were plotted on maps and related to possible sources of pollutants. Our results indicate that hydrothermal fluid circulation and the water–rock interaction of country rocks that host mineralized ore deposits generate a significant flux of heavy metals to groundwater, as well as anthropogenic sources like intense agriculture and industrial activities. In particular, NO3, F, and Ni exceed the Maximum Admitted Concentrations (MACs) established by the WHO and Italian legislation for drinking-water. The spatial distributions of geogenic and anthropogenic sources were so deeply interlocked that their separation was not easy, also employing geostatistical tools. This complex scenario makes the implementation of human health risk mitigation actions difficult, since the flow of pollutants is in many cases controlled by simple water–rock interaction processes.
机译:我们从Barcellona-Milazzo平原(意大利西西里岛最重要的沿海含水层之一)的井中收集并分析了58个地下水样品,以确定主要,次要和痕量元素的浓度。在该地区,重金属和其他污染物的地源和人为源共同作用,使得主要污染源难以区分。我们的工作旨在应用地统计学标准来区分这些污染源。我们使用概率图从背景浓度中分离出异常值,将其绘制在地图上并与可能的污染物来源相关。我们的研究结果表明,热液循环和承载矿化矿床的乡村岩石的水-岩相互作用会产生大量重金属向地下水,以及诸如农业和工业活动之类的人为源。特别是,NO3,F和Ni超过了WHO和意大利关于饮用水的法规所规定的最大允许浓度(MACs)。地源和人为源的空间分布是如此紧密地联系在一起,以致于它们的分离并不容易,而且还使用了地统计学工具。这种复杂的情况使实施减轻人类健康风险的措施变得困难,因为在许多情况下,污染物的流动受简单的水-岩相互作用过程控制。

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