利用延时二维和三维地电反演模型监测酸性矿井排水——以实例为例

B. Jodeiri Shokri, Foojan Shafaei, F. Doulati Ardejani, A. Mirzaghorbanali, Sh. Entezam
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引用次数: 3

摘要

洗煤厂产生大量废弃物,尾矿一般倾倒在洗煤厂附近的堆积场和蓄水池中。硫化物矿物、水渗透和氧扩散可导致酸性矿井排水(AMD)。本文采用延时二维和三维地电技术对伊朗东北部一家洗煤厂产生的AMD进行了监测研究。为此,利用偶极-偶极阵列在废弃桩周围和两个蓄水池附近进行了二维和三维地电测量。这些调查在第一次测量后六个月重复进行,以表征介质的时间变化。二维地电延时显示,AMD是在桩的较浅水平产生的。此外,三维时移和水文地球化学分析表明,可能的羽流被输送到桩基下游的地下水中。此外,延时三维地电模型的结果表明,季节变化(主要是降水)可能会影响可能的羽流并将其输送到次表层。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Use of time-lapse 2D and 3D geoelectrical inverse models for monitoring acid mine drainage -a case study
ABSTRACT Coal washing plants produce large amounts of waste, and tailings are generally dumped in piles and impoundments nearby the plants. Sulfide minerals, water infiltration, and oxygen diffusion can result in acid mine drainage (AMD). In this paper, monitoring the AMD generated by a coal washing plant in northeastern Iran was investigated by applying time-lapse 2D and 3D geoelectrical techniques. For this purpose, 2D and 3D geoelectrical surveys with the Dipole-Dipole array were conducted in the area surrounded by an abandoned pile and nearby two impoundments. The surveys were repeated six months after the first measurements to characterize the temporal changes in the medium. 2D geoelectrical time-lapse suggests that the AMD is being generated at the shallower level of the pile. Moreover, the 3D time-lapse and hydrogeochemical analysis indicate that the likely plume is conveyed to the groundwater downstream of the pile. Besides, the results of time-lapse 3D geoelectrical models illustrate that seasonal changes, mainly precipitation, could affect the likely plume and transport it to subsurface layers.
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