Trace elements in water, sediments, porewater, and biota polluted by tailings from an abandoned gold mine in British Columbia, Canada
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Activation and utilization of tailings as CO<inf>2</inf> mineralization feedstock and supplementary cementitious materials: a critical review
2023, Materials Today SustainabilityPhysical and chemical characterization of sediments from an Andean river exposed to mining and agricultural activities: The Moquegua River, Peru
2022, International Journal of Sediment ResearchCitation 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 PollutionCitation 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 ManagementCitation 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 EnvironmentCitation 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