Faculty of Natural Sciences, University of Silesia, 60 Będzińska St., PL-41-200, Sosnowiec, Poland.
Institute of Environmental Engineering, Polish Academy of Sciences, 34 Skłodowskiej-Curie St., PL-41-819, Zabrze, Poland.
Environ Sci Pollut Res Int. 2020 May;27(14):16731-16744. doi: 10.1007/s11356-020-08195-4. Epub 2020 Mar 4.
Long-term underground exploitation of Zn-Pb ores has led to drainage of the area and formation of a huge dumping ground in the form of a pile. In its vicinity, processes of acid drainage have developed as a result of contamination of soils and groundwater. Geochemical transformations of mineral contents of waste can significantly affect physical and chemical properties of the soils and the bedrock. At the prospect of termination of the mining activity in the near future, determining the routes of the pollution migration, ability to monitor acid drainage processes and assessment of the risk of heavy metal pollution are really crucial. The paper presents a proposal for solving this problem by means of geophysical methods: Electrical Resistivity Tomography (ERT), Time Domain-Induced Polarisation (TDIP), Frequency Domain Electromagnetics (FDEM) and shallow-depth magnetometric surveys combined with geochemical investigations. The obtained results of geophysical surveys have been confirmed by geochemical investigations. The applied ERT and TDIP methods make it possible to identify the spread of the zones of pollution around the tailing pile, but their effectiveness depends on humidity of the ground. Soil magnetometry and shallow-depth induction profiling are a good tool to identify the medium contaminated with minerals redeposited by aeolian processes and allow to determine the range of the dust spread from the pile. It has been shown that the range of impact of the geochemical changes around the tailing pile is high and depends not only on directions and dynamics of water flow from the pile but also on aeolian transport.
长期以来对 Zn-Pb 矿的地下开采导致了该地区的排水,并形成了一个巨大的堆积物形式的倾倒场。在其附近,由于土壤和地下水的污染,已经形成了酸性排水的过程。废物中矿物含量的地球化学转化会显著影响土壤和基岩的物理和化学性质。在不久的将来即将停止采矿活动的情况下,确定污染迁移的路径、监测酸性排水过程的能力以及评估重金属污染的风险确实至关重要。本文提出了一种通过地球物理方法解决此问题的建议:电阻率层析成像(ERT)、时域激发极化(TDIP)、频率域电磁法(FDEM)和浅层磁力测量与地球化学调查相结合。地球物理调查的结果得到了地球化学调查的证实。所应用的 ERT 和 TDIP 方法可以识别尾矿堆周围污染区的扩散,但它们的有效性取决于地面的湿度。土壤磁测和浅层感应剖面是识别被风成过程重新沉积的矿物污染的良好工具,并允许确定从堆中散布的灰尘范围。结果表明,尾矿堆周围地球化学变化的影响范围很大,不仅取决于从堆中流出的水流的方向和动态,还取决于风的输送。