2005
DOI: 10.1016/j.gca.2004.10.031
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Mineral/water interactions in tailings from a tungsten mine, Mount Pleasant, New Brunswick

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Cited by 39 publications
(12 citation statements)
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“…One of our research interests is related to the oxidation of arsenopyrite (FeAsS) in the tailings from the Mount Pleasant Tungsten Mine, which is located approximately 60 km south of Fredericton, NB. The geochemistry, hydrogeology, and mineralogy of the Mount Pleasant Mine tailings has been previously presented by Petrunic and Al (2005), and from this study it is evident that elevated As concentrations occur in the near-surface pore water (maximum of 7.1 mg/L). The abiotic and biotic oxidation of arsenopyrite under a variety of conditions (e.g., air and aqueous solutions) has been studied previously (e.g., Buckley and Walker 1988;Richardson and Vaughan 1989;Nesbitt et al 1995;Fernandez et al 1996a, b;Nesbitt and Muir 1998;Schaufuss et al 2000;Jones et al 2003;Mikhlin and Tomashevich 2005).…”
Section: Introductionsupporting
confidence: 56%
“…One of our research interests is related to the oxidation of arsenopyrite (FeAsS) in the tailings from the Mount Pleasant Tungsten Mine, which is located approximately 60 km south of Fredericton, NB. The geochemistry, hydrogeology, and mineralogy of the Mount Pleasant Mine tailings has been previously presented by Petrunic and Al (2005), and from this study it is evident that elevated As concentrations occur in the near-surface pore water (maximum of 7.1 mg/L). The abiotic and biotic oxidation of arsenopyrite under a variety of conditions (e.g., air and aqueous solutions) has been studied previously (e.g., Buckley and Walker 1988;Richardson and Vaughan 1989;Nesbitt et al 1995;Fernandez et al 1996a, b;Nesbitt and Muir 1998;Schaufuss et al 2000;Jones et al 2003;Mikhlin and Tomashevich 2005).…”
Section: Introductionsupporting
confidence: 56%
“…However, if we assume that Al and Fe concentrations in these reactors equaled the detection limits of the method (0.1 and 0.9 lmol/L, respectively), then we estimate that abundances of Al-F and Fe-F complexes in the biotic reactors exceeded those in the control reactors by $3 to 5 and 1-2 orders of magnitude, respectively. Formation of Al-F and Fe-F complexes can enhance the solubility and dissolution rate of Al-and Fe-bearing minerals by lowering the activities of Al and Fe in solution (Pulfer et al, 1984;Ž utić and Stumm, 1984;Plankey et al, 1986;Haidouti, 1995;Phillips et al, 1997;Kraemer et al, 1998;Nordin et al, 1999;Harouiya and Oelkers, 2004;Wolff-Boenisch et al, 2004;Petrunic and Al, 2005). Our experiments therefore point to a potentially important bioweathering mechanism where actively metabolizing heterotrophic bacteria increase Al, and to a lesser extent, Fe release from granite by first accelerating the dissolution of co-existing, F-bearing trace phases.…”
Section: Elemental Release Ratesmentioning
confidence: 67%
“…These characteristics include: mineralogical and geochemical compositions; specific gravity of tailings particles; settling behaviour; permeability vs. density relationships; soil plasticity (i.e. Laboratory methods for the mineralogical and geochemical analysis of tailings solids and waters are given by Jambor (1994), Crock et al (1999), andPetruk (2000). Detailed procedures for tailings sampling, preparation and analysis are found in Ficklin and Mosier (1999).…”
Section: Tailings Characteristicsmentioning
confidence: 99%