Electrical Resistivity Imaging Applied to Mining Legacy Site

A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Environmental Mineralogy and Biogeochemistry".

Deadline for manuscript submissions: closed (30 September 2023) | Viewed by 1434

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Department of Mining and Civil Engineering, Universidad Politécnica de Cartagena, 30203 Cartagena, Spain
Interests: applications of electrical, seismic, and electromagnetic techniques focused on near-surface characterization in environmental, mining, and hydrogeological research

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Department of Civil and Mining Engineering, Technical University of Cartagena, 30203 Cartagena, Spain
Interests: applications of electrical, seismic, and electromagnetic techniques focused on near-surface characterization in environmental, mining, and hydrogeological research
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Oulu Mining School, University of Oulu, 90570 Oulu, Finland
Interests: multi-source data fusion integrating earth observation, airborne-, and ground-based geophysics in mining environments

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Department of Mechanical and Mining Engineering, EPS Linares and CEACTEMA, University of Jaén, Technological Scientific Campus, 23700 Linares, Spain
Interests: applications of electrical, magnetic, and electromagnetic techniques focused on near-surface characterization in environmental, mining, and hydrogeological research

Special Issue Information

Dear Colleagues,

Electrical resistivity imaging (ERI) is a non-destructive geophysical technique used to measure and map the distribution electrical resistivity of different materials in the subsurface. Thus, ERI can delineate zones in the subsurface with distinctive electrical resistivity values, and this capability has been used extensively in several applications across industries.

This field of application has increasingly been applied for the past 30 years for mapping the subsurface of mining legacy sites or so-called abandoned mines. The subsurface of mining areas can host minerals that are prone to other physical and chemical processes by which the structure and properties of the ground, pore water, and groundwater can be altered. The result of this interaction can lead to geochemical reactions increasing the acidity and salinity at specific zones of the subsurface which can be determined using a proxy measurement such as electrical resistivity.

In most cases, ERI was applied in mining waste and tailings (e.g., for mapping the structure of embankments and seepage pathways), which are often associated with environmental and human health concerns due to the potential for contaminant release. ERI has also been used in mining legacy sites in conjunction with other geophysical techniques (e.g., IP, SP, electromagnetic induction, active and seismic imaging, and ground penetrating radar) to interpret other processes related to the stratigraphy, geochemistry, and hydrogeology of the subsurface.

There are several advantages in using ERI in mining legacy sites. ERI is non-invasive technique that does not require drilling or excavation, making it a cost-effective and safe method with only a few hours to complete field data acquisition. It can provide high-resolution imagery and therefore detailed mapping of the subsurface. It is flexible as it can be applied in a variety of environments including land and water. In addition, ERI is a low-impact geophysical technique as it does not cause significant noise or disturb the environment, making it a preferred option for sensitive environments.

As for assisting the monitoring and management of mining legacy sites, ERI can offer a wide range of applications such as environmental site assessments, identifying the extent of contaminated land areas, phreatic water, and groundwater, allowing for a better targeting of remediation efforts. ERI can be used to monitor the effectiveness of remediation by mapping changes in subsurface electrical resistivity over time, allowing for the identification of changes in the distribution of contaminants. ERI can also be used to assess the stability of mining waste deposits by identifying areas of low electrical resistivity associated with the presence of saturated materials or zones of weakness. Other ERI applications can include mapping geochemical processes and, potentially, mineral exploration in mining secondary resources.

Dr. Marcos Antonio Martínez-Segura
Prof. Dr. Pedro Martínez-Pagán
Dr. Raul Mollehuara Canales
Dr. Rosendo Mendoza Vílchez
Guest Editors

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Keywords

  • electrical resistivity imaging
  • tailing dam
  • orphan mines, derelict mines, mining legacy sites, abandoned mines
  • environmental contamination
  • environmental remediation
  • geotechnical stability
  • potential mineral exploration
  • mining secondary resources

Published Papers (1 paper)

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Research

19 pages, 24317 KiB  
Article
Mapping Leachate Pathways in Aging Mining Tailings Pond Using Electrical Resistivity Tomography
by Mosaad Ali Hussein Ali, Farag M. Mewafy, Wei Qian, Fahad Alshehri, Sattam Almadani, Mofleh Aldawsri, Majed Aloufi and Hussein A. Saleem
Minerals 2023, 13(11), 1437; https://doi.org/10.3390/min13111437 - 13 Nov 2023
Cited by 2 | Viewed by 990
Abstract
Mining activities often leave behind a legacy of environmental challenges, with aging tailings ponds representing a significant concern due to their potential for leachate formation and subsequent contaminant release. Thus, this study employs Electrical Resistivity Tomography (ERT) to investigate the intricate pathways of [...] Read more.
Mining activities often leave behind a legacy of environmental challenges, with aging tailings ponds representing a significant concern due to their potential for leachate formation and subsequent contaminant release. Thus, this study employs Electrical Resistivity Tomography (ERT) to investigate the intricate pathways of leachate within an aging mining tailings pond, addressing the pressing environmental and human health concerns associated with potential contaminant release. Ten 2D ERT profiles were acquired at the El Mochito mine waste site, covering an area of approximately half a square kilometer. These profiles, ranging in length from 104 to 363 m, provided insights into subsurface conditions down to a maximum depth of 60 m. The subsurface mapping of the ERT data showed three different geoelectric layers. The uppermost layer, with a thickness of approximately 2.5 m and resistivity values ranging from 60 to 100 Ohm.m, was identified as a dry tailing/soil zone. Beneath it, the second layer exhibited moderately resistive values (30–60 Ohm.m) with varying thicknesses of 10–20 m, signifying a percolation/leaching zone (semi-saturated zone). The third layer, characterized by substantially low resistivity (1–30 Ohm.m), indicated saturation and the presence of conductive materials, strongly suggesting active leaching. Based on these findings, this study recommends further investigation through geochemical analysis of subsurface samples and more advanced geophysical imaging techniques to validate the distribution of anomalous zones and delineate remediation pathways. This study lays the foundation for future comprehensive research that will integrate geophysical surveys with geochemical analysis and establish 4D modeling techniques to monitor pollutant penetration over time, with a particular focus on mine waste tailings mapping. Plus, this study contributes valuable insights into the characterization of leachate pathways within mining tailings ponds, offering a foundation for informed environmental management and remediation strategies. Full article
(This article belongs to the Special Issue Electrical Resistivity Imaging Applied to Mining Legacy Site)
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