Trace elements in water, sediments, porewater, and biota polluted by tailings from an abandoned gold mine in British Columbia, Canada

https://doi.org/10.1016/0375-6742(94)00028-AGet rights and content

Abstract

The concentrations of major and trace elements in different environmental compartments (e.g., water, suspended and bottom sediments, sediment porewater, and biota) of Jack of Clubs Lake (JCL), Wells, British Columbia (Canada), were determined to assess the biogeochemical effects of abandoned gold mine tailings on the aquatic ecosystem of JCL in the Fraser River drainage basin. Arsenic and Pb were transported from the tailings to the lake, where they accumulated in bottom sediments in concentrations up to 1104 and 281 μ/g, respectively. Although the benthic community in the lake was only partially affected, there was evidence that the tailings inhibited a variety of microbial activities in the lake sediments. The concentrations of As, Cd, Cu and Pb in invertebrates collected from streams flowing through mine tailings, and from vegetation growing on the tailings, suggest a potential for contamination of the food chain of the surrounding ecosystems.

References (30)

  • J.M. Besser et al.

    Bioavailability and toxicity of metals leached from lead-mine tailings to aquatic invertebrates

    Environ. Toxicol. Chem.

    (1987)
  • R.L. Cowie et al.

    Pulmonary tuberculosis in South African gold miners

    Am. Rev. Respir. Dis.

    (1989)
  • C. Finch et al.

    Curr. Res. Newfoundland Dep. Mines Energy

    (1992)
  • D.M. Galbraith

    Reclamation assessment — Wells tailings

    (1991)
  • G.B. Halverson et al.

    Treatment of and recovery from effluent at Giant Yellowknife Mines Limited

    Water Pollul. Res. J. Can.

    (1987)
  • Cited by (55)

    • Physical and chemical characterization of sediments from an Andean river exposed to mining and agricultural activities: The Moquegua River, Peru

      2022, International Journal of Sediment Research
      Citation Excerpt :

      A similar situation could also occur in Moquegua; since both plants are found on the banks of the Moquegua River. On the other hand, arsenic is always found in areas where Cu mining companies operate (Ashley & Lottermoser, 1999; Azcue et al., 1995; Azcue & Nriagu, 1995; Bissen & Frimmel, 2003; Cancès et al., 2008; Davis et al., 1992; Foster et al., 1998; Hudson et al., 1997; Nesbitt & Muir, 1998; Ondrus et al., 1997; Paktunc et al., 2004; Utsunomiya et al., 2003; Williams et al., 1996) and Moquegua is not an exception. In this work, arsenic and arsenic forming alarsite (AlAsO4) and arsenolite (As2O3) has been found in samples from many study sites in the lower drainage basin and the headwaters of the Torata River, above the Cuajone mine.

    • Lead contamination from gold mining in Yellowknife Bay (Northwest Territories), reconstructed using stable lead isotopes

      2020, Environmental Pollution
      Citation Excerpt :

      Mining-derived Pb was deposited at the north end of the bay from atmospheric deposition, solid tailings or effluent flowing down Baker Creek, and a small fraction of this pollution then likely moved slowly southward over time by sediment migration. We measured sediment Pb concentration gradients comparable to those reported for lakes near Canadian gold mines but well below the reported values for sediment in tailing ponds for the same mines (Mudroch et al., 1989; Azcue et al., 1995; Wong et al., 1999). The maximum mining-derived Pb flux reported in this study (63 mg m−2 yr−1) was comparable to the maximum recorded Pb fluxes from lakes located between 6 and 36 km from copper smelter of the Rouyn-Noranda mining area (27–58 mg m−2 yr−1) (Couillard et al., 2008; Gallon et al., 2006).

    • Arsenic and antimony in water and wastewater: Overview of removal techniques with special reference to latest advances in adsorption

      2015, Journal of Environmental Management
      Citation Excerpt :

      Arsenic concentrations in lake waters are usually close to or lower than those found in river water (Smedley and Kinniburgh, 2002). Baseline concentrations are typically bellow 1 μg/L or near 1–2 μg/L (Azcue et al., 1994, 1995; Azcue and Nriagu, 1995; Ikem and Egilla, 2008; Mannio et al., 1995; Reuther, 1992), but values in the range 1–157 μg/L have been reported in lakes of different countries, as for example Lake Mohawk (USA), two lakes of China and in south east part of Sindh, Pakistan (Arain et al., 2009; Barringer et al., 2011). The antimony distribution in natural waters has received much less attention than arsenic.

    • Individual and cumulative effects of agriculture, forestry and metal mining activities on the metal and phosphorus content of fluvial fine-grained sediment; Quesnel River Basin, British Columbia, Canada

      2014, Science of the Total Environment
      Citation Excerpt :

      In some cases, average values for impacted sites are significantly (p < 0.05) greater than reference sites, for example: (i) Mn for agricultural sites; (ii) As, Hg, P and Se for mining sites; and (iii) Cu, Hg, Pb and Zn for forestry sites. Both As and Se are by-products of the Cu and Ag mining processes (Azcue et al., 1995; Korte and Coulston, 1998; Luoma and Rainbow, 2008), which likely explains their elevated levels. In the case of forestry practices, Cu-rich local geology may have been disturbed and transported during forestry practices resulting in elevated levels for that land use (Hassan et al., 2005).

    • Arsenic and Selenium

      2013, Treatise on Geochemistry: Second Edition
    View all citing articles on Scopus
    View full text