3D TIME-LAPSE GEOELECTRICAL MONITORING OF MOISTURE CONTENT IN AN EXPERIMENTAL WASTE ROCK PILE: VALIDATION USING HYDROGEOLOGICAL DATA

Adrien Dimech, M. Chouteau, V. Martin, M. Aubertin, B. Bussière, B. Plante
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引用次数: 8

Abstract

The hydrogeological behavior of heterogeneous and unsaturated media can be challenging to assess, especially where classical hydrogeological instrumentation cannot be directly installed such as in the core of waste rock piles. In this paper, the authors present the results of several 3D Electrical Resistivity Tomography surveys carried out in 2017 for time-lapse monitoring of water infiltration events in an experimental waste rock pile. This pile was built according to a recently proposed waste rock disposal method at the Lac Tio mine (RTFT, Québec, CA) that aims at diverting water flow from potentially reactive waste rock, thus limiting metal leaching and contamination of the effluent. The pile has been instrumented with soil moisture sensors and lysimeters to monitor water content over time and collect percolating water. In addition, 192 buried electrodes have been used to carry hourly measurements with an optimized protocol of 1000 configurations uploaded on a Terrameter LS (ABEM) to monitor internal flow of water sprinkled on the top of the pile with a water truck. Time-lapse 3D ERT data were inverted to yield the 3D model of soil electrical resistivity over time before, during and after induced infiltration events in the pile. While resistivity results show consistent variations associated with increased moisture content, conversion of resistivity into volumetric water content is not straightforward. This challenge is related, in part, to changes in the distribution of water resistivity over time in the pile, which in turn strongly affects resistivity within the waste rock. Laboratory column measurements have been conducted to assess the relationship between global (waste rock) resistivity, water resistivity and moisture content for samples from the pile. The images of water content obtained with ERT are then validated with hydrogeological measurements and modeling of the pile. This assessment indicates that geoelectrical monitoring is an efficient tool to monitor water moisture in a complex media.
三维时移地电监测实验废石桩含水率:利用水文地质数据验证
非均质和非饱和介质的水文地质行为很难评估,特别是在不能直接安装经典水文地质仪器的地方,如废石桩的核心。在本文中,作者介绍了2017年进行的几次三维电阻率层析成像调查的结果,用于对实验废石堆中的水渗透事件进行延时监测。这桩桩是根据最近在Lac Tio矿(RTFT, quacimubec, CA)提出的废石处理方法建造的,该方法旨在从可能发生反应的废石中分流水流,从而限制金属浸出和废水污染。桩上装有土壤湿度传感器和渗滤仪,以监测一段时间内的含水量并收集渗水。此外,192个埋在地下的电极每小时进行一次测量,并将1000个配置的优化方案上传到Terrameter LS (ABEM)上,以监测用水车洒在桩顶的水的内部流动。对延时三维ERT数据进行反演,得到桩内诱发入渗事件发生前、中、后土层电阻率随时间变化的三维模型。虽然电阻率结果显示与含水量增加相关的一致变化,但将电阻率转换为体积含水量并不简单。这一挑战部分与桩中水电阻率随时间分布的变化有关,这反过来又强烈影响废石中的电阻率。已进行了实验室柱测量,以评估桩样的整体(废石)电阻率、水电阻率和水分含量之间的关系。然后用水文地质测量和桩的建模来验证ERT获得的含水率图像。这一评价表明,地电监测是监测复杂介质中水分的有效工具。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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