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    Characterization of Tailings Dust from Two Abandoned Mine Sites: Effects on Nearby Surface Waters and Evaluation of Dust Sampling Methods

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    Thesis Document (8.128Mb)
    Dust Deposition Gauge Results (75.45Kb)
    Dust-Water Ratio Investigation (57.80Kb)
    EMP Results (111.8Kb)
    Filter Weights and Deposition Rates (66.30Kb)
    HVAS Flow Rates (20.90Kb)
    Lichen Results (75.71Kb)
    MLA Results and Mass Distribution Calculations (80.18Kb)
    Pas-DD and HVAS Aqua Regia ICP-AES Results (151.2Kb)
    Pas-DD and HVAS Aqua Regia ICP-MS Results (256.7Kb)
    Pas-DD and HVAS Shake Flask ICP-AES Results (272.1Kb)
    Pas-DD and HVAS Shake Flask ICP-MS Results (263.7Kb)
    Stream Water Results and PHREEQC Input (87.63Kb)
    Tailings Aqua Regia ICP-AES Results (171.0Kb)
    Tailings Aqua Regia ICP-MS Results (32.90Kb)
    Tailings Shake Flask ICP-AES Results (29.81Kb)
    Tailings Shake Flask ICP-MS Results and PHREEQC Input (31.93Kb)
    Weather (34.25Kb)
    Author
    Cleaver, Amy
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    Abstract
    Canada’s climate is warming and as a result the hydrological cycle is expected to become more intense, with rainfall concentrated in extreme events with longer dry spells. Consequently, dry tailings may be more likely to blow into nearby surface waters. This research is an investigation into the geochemical effects of tailings dust on nearby surface waters and evaluates dust sampling methods used to investigate seasonal trends. During this study, two abandoned mine sites in Nova Scotia, Canada were investigated: Stirling Zn-Pb and Goldenville Au mine.

    At Stirling, tailings were sieve to <63μm as a proxy for dust and analyzed to determine metal concentrations and identify primary and secondary metal-bearing phases. Metal-hosting phases identified include sphalerite, smithsonite, aurichalcite, hydrohetaerolite, goethite. tennantite, galena, cerussite, Pb-Mn phases, and chalcopyrite. Shake flask tests were conducted to investigate dust solubility in simulated stream waters (pH=7). Results indicate that dust particles are partially water soluble in the shake flask test and that sphalerite, cerussite and chalcopyrite are likely the main sources of Zn, Pb and Cu in the shake flask leachate, based on calculated saturated indices and mass balance. Analyses of stream water indicate similar conditions (pH, Eh, etc.) and saturation indices compared to shake flask tests, and therefore provide reasonable insight for processes occurring the field.

    Dust was also sampled using a variety of different methods to identify the most suitable method for seasonal sampling. These included passive dry deposition collectors (PAS-DDs), high volume total suspended particle (TSP) sampler (HVAS), dust deposition gauges (DDGs), and lichen. Results indicate that Pas-DDs with a glass fiber filters (GFF) and dust deposition gauges likely underestimate dust deposition. In comparison, Pas-DDs with a polyurethane foam disk (PUF) efficiently accumulate dust. However, PUFs had additional challenges including metal(loid)s within the filters themselves, difficulty obtaining stable weights, and potential dust collection from the sides and bottom. Despite difference between dust sampling methods, it was observed that dust deposition was highest in the winter months due to higher wind speeds. Future dust generation remains difficult to predict due to the unknown combined effect of changes in temperature, precipitation, evaporation, and wind speed.
    URI for this record
    http://hdl.handle.net/1974/27960
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    • Department of Geological Sciences and Geological Engineering Graduate Theses
    • Queen's Graduate Theses and Dissertations
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