Abstract
Potential problems related to a tailings dam’s stability are a matter of concern, especially where structural failure might endanger nearby communities and the environment. The Osamu Utsumi mine, located in the State of Minas Gerais, is currently not operating. The rock-soil tailings dam has water upwelling downstream in the bedrock, with water flux confined to rock fractures. This research was conducted to identify possible flux zones in the base of the dam using DC resistivity and electrical resistivity tomography (ERT). The data acquisition consisted of five ERT lines with 6 m of spacing between electrodes, using a Schlumberger array. The results are presented by 2D and 3D geophysical models comprising measured and processed resistivity values. It was possible to identify a low resistivity zone (5–20 Ωm), whose structural continuity indicates water infiltration in the bedrock under the dam. Moreover, the results do not indicate that erosion is taking place in the interior of the dam, reducing the risk of geotechnical instability and failure of physical integrity.
Resumen
Los potenciales problemas relacionados con la estabilidad de un dique de colas son motivo de preocupación, especialmente cuando una falla estructural puede poner en peligro a las comunidades aguas abajo y al medio ambiente. La mina Osamu Utsumi, situada en el Estado de Minas Gerais (Brasil), no está actualmente en operación. La presa de relaves de roca-suelo tiene flujo hídrico con aguas surgentes aguas abajo, en el lecho rocoso, relacionadas y restringidas a las fracturas del substrato rocoso. Esta investigación se llevó a cabo para identificar posibles franjas de flujo, en el basamento de la presa, utilizando resistividad DC y tomografía de resistividad eléctrica (ERT). El registro de datos se efectuó en cinco líneas de ERT, con 6 m de espaciado entre electrodos, utilizando el dispositivo Schlumberger. Los resultados se presentan en modelos geofísicos 2D y 3D, que incluyen valores de resistividad medidos y procesados. La investigación permitió identificar una franja de baja resistividad (5–20 Ωm), cuya continuidad estructural refleja la infiltración y flujo de agua en el substrato rocoso, bajo la presa. Además, los resultados no manifiestan que se esté produciendo erosión en el cuerpo de la presa, lo que reduce el riesgo de inestabilidad geotécnica y de fallo de su integridad física.
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The authors thank the Foundation for Research Support of the State of Sao Paulo (Fundação de Amparo a Pesquisa do Estado de São Paulo—FAPESP process No. 2018 / 14565-3) and the INB for the support.
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Arcila, E.J.A., Moreira, C.A., Camarero, P.L. et al. Identification of Flow Zones Inside and at the Base of a Uranium Mine Tailings Dam Using Geophysics. Mine Water Environ 40, 308–319 (2021). https://doi.org/10.1007/s10230-020-00746-y
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DOI: https://doi.org/10.1007/s10230-020-00746-y