A multiscale accuracy assessment of moisture content predictions using time-lapse electrical resistivity tomography in mine tailings

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作者
Adrien Dimech
Anne Isabelle
Karine Sylvain
Chong Liu
LiZhen Cheng
Bruno Bussière
Michel Chouteau
Gabriel Fabien-Ouellet
Charles Bérubé
Paul Wilkinson
Philip Meldrum
Jonathan Chambers
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[1] Université du Québec en Abitibi-Témiscamingue (UQAT),
[2] Polytechnique Montréal,undefined
[3] Research Institute of Mines and Environment (RIME),undefined
[4] British Geological Survey (BGS),undefined
[5] Environmental Science Centre,undefined
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Accurate and large-scale assessment of volumetric water content (VWC) plays a critical role in mining waste monitoring to mitigate potential geotechnical and environmental risks. In recent years, time-lapse electrical resistivity tomography (TL-ERT) has emerged as a promising monitoring approach that can be used in combination with traditional invasive and point-measurements techniques to estimate VWC in mine tailings. Moreover, the bulk electrical conductivity (EC) imaged using TL-ERT can be converted into VWC in the field using petrophysical relationships calibrated in the laboratory. This study is the first to assess the scale effect on the accuracy of ERT-predicted VWC in tailings. Simultaneous and co-located monitoring of bulk EC and VWC are carried out in tailings at five different scales, in the laboratory and in the field. The hydrogeophysical datasets are used to calibrate a petrophysical model used to predict VWC from TL-ERT data. Overall, the accuracy of ERT-predicted VWC is ±0.03m3/m3\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$\pm 0.03~\textrm{m}^3/\textrm{m}^3$$\end{document}, and the petrophysical models determined at sample-scale in the laboratory remain valid at larger scales. Notably, the impact of temperature and pore water EC evolution plays a major role in VWC predictions at the field scale (tenfold reduction of accuracy) and, therefore, must be properly taken into account during the TL-ERT data processing using complementary hydrogeological sensors. Based on these results, we suggest that future studies using TL-ERT to predict VWC in mine tailings could use sample-scale laboratory apparatus similar to the electrical resistivity Tempe cell presented here to calibrate petrophysical models and carefully upscale them to field applications.
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