An integrated investigation of the Rio tailings, Panasqueira mine, Centre Portugal

The risks associated with mine tailings have different nature and, thus, only a multiple approach can investigate and monitor comprehensively the characteristics and evolution of mine tailings impacts on the environment. Deposition at the Rio tailings (Panasqueira Mine) lasted about ninety years. Over one million cubic metres, of complex very fine to fine material, are deposited on a mountain side overlaying the Zezere river, increasing the risk of contamination of one of the most important hydrographic basins in central Portugal. Herein, a multidisciplinary study including geophysics, geochemistry and borehole information, organized in a GIS, is used to characterize the Rio tailings. The geophysical survey comprised ERT (Electrical Resistivity Tomography) and GPR (Ground Penetrating Radar) on the mud impoundment, as well as, on the slope of the tailings. The geochemical survey consisted on collecting water and tailings samples, iron coatings, arsenopyrite stockpile material and ferruginous crust. Samples collected in boreholes, drilled specifically for this project, were also analyzed. The GIS provided imaging of the geophysical, geochemical and particle size spatial distribution, so that comparisons between the different data sets are easily done. Resistivity and GPR allowed bedrock positioning. GPR was able to give layering results within the tailings. Finally, comparison and correlation between geophysical and geochemical results are carried out and evaluated on the GIS platform. Key word: mine, geophysics, tailings, geochemistry, contamination, structure, risk

[1]  M. Chouteau,et al.  Geophysical experiments to image the shallow internal structure and the moisture distribution of a mine waste rock pile , 2009 .

[2]  J. Farinha,et al.  Geochemistry and Mineralogy of Mill Tailings Impoundments from the Panasqueira Mine (Portugal): Implications for the Surrounding Environment , 2008 .

[3]  Alexandre Lourenço As Minas da Panasqueira , 2008 .

[4]  Sam Johansson,et al.  Detection of Internal Erosion and Seepage Using Resistivity Monitoring , 2007 .

[5]  J. D. Rnrsrtor The solubility and stability of scorodite, , 2007 .

[6]  Sam Johansson,et al.  Using resistivity measurements for dam safety evaluation at Enemossen tailings dam in southern Sweden , 2005 .

[7]  V. McLemore,et al.  NEAR SURFACE GEOPHYSICS FOR THE STRUCTURAL ANALYSIS OF A MINE ROCK PILE, NORTHERN NEW MEXICO , 2005 .

[8]  P. Gélinas,et al.  Geochemical characterization of acid mine drainage from a waste rock pile, Mine Doyon, Québec, Canada. , 2004, Journal of contaminant hydrology.

[9]  M L de la Torre,et al.  Odiel River, acid mine drainage and current characterisation by means of univariate analysis. , 2003, Environment international.

[10]  L. Fontboté,et al.  Element cycling and secondary mineralogy in porphyry copper tailings as a function of climate, primary mineralogy, and mineral processing , 2001 .

[11]  S. Brake,et al.  A river runs through it: impact of acid mine drainage on the geochemistry of West Little Sugar Creek pre- and post-reclamation at the Green Valley coal mine, Indiana, USA , 2001 .

[12]  T. V. Panthulu,et al.  Detection of seepage paths in earth dams using self-potential and electrical resistivity methods , 2001 .

[13]  F. Frau The formation-dissolution-precipitation cycle of melanterite at the abandoned pyrite mine of Genna Luas in Sardinia, Italy: environmental implications , 2000, Mineralogical Magazine.

[14]  D. L. Campbell,et al.  Geoelectrical laboratory measurements of materials from the May Day Mine dump, southwestern Colorado , 2000 .

[15]  D. Nordstrom,et al.  Negative pH, efflorescent mineralogy, and consequences for environmental restoration at the Iron Mountain Superfund site, California. , 1999, Proceedings of the National Academy of Sciences of the United States of America.

[16]  T. Valente,et al.  Tipologia e evoluçao dos materiais de neoformaçao supergénica detectados na escombreira da Mina de Valdarcas (Vila Nova da Cerveira, N Portugal): implicaçoes ambientais , 1998 .

[17]  Douglas Yuval,et al.  DC resistivity and IP methods in acid mine drainage problems: results from the Copper Cliff mine tailings impoundments , 1996 .

[18]  R. Barker,et al.  Rapid least-squared inversion of apparent resisitivity pseudosections by a quasi-Newton method , 1996 .

[19]  Kathleen S. Smith,et al.  Geoenvironmental models of mineral deposits, and geology-based mineral-environmental assessments of public lands , 1994 .

[20]  K. White,et al.  Metal transport in a stream polluted by acid mine drainage--The Afon Goch, Anglesey, UK. , 1994, Environmental pollution.

[21]  Armanda Dória,et al.  Characterization and timing of the different types of fluids present in the barren and ore-veins of the W-Sn deposit of Panasqueira, Central Portugal , 1992 .

[22]  M. Hamburger,et al.  A STUDY OF ACID MINE DRAINAGE USING EARTH RESISTIVITY MEASUREMENTS , 1990 .

[23]  A. A. Hammond,et al.  Mining and quarrying wastes: A critical review , 1988 .

[24]  P. Dove,et al.  The solubility and stability of scorodite, FeAsO 4 .2H 2 O , 1985 .

[25]  R. Rye,et al.  Geologic, fluid inclusion, and stable isotope studies of the tin-tungsten deposits of Panasqueira, Portugal , 1979 .

[26]  I. Jonasson,et al.  The geochemistry of arsenic and its use as an indicator element in geochemical prospecting , 1973 .

[27]  M. Loke Electrical Imaging Surveys for Environmental and Engineering Studies , 2022 .