4.5 Article

Subsurface variations in arsenic mineralogy and geochemistry following long-term weathering of gold mine tailings

Journal

APPLIED GEOCHEMISTRY
Volume 73, Issue -, Pages 81-97

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.apgeochem.2016.07.013

Keywords

Arsenic; Mine waste; Mineralogy; Gold; Remediation; Nova Scotia

Funding

  1. NSERC Metals in the Human Environment Strategic Network (MITHE-SN)
  2. NSERC Strategic Grant [364927]
  3. Environmental Geoscience Program of the Earth Sciences Sector at Natural Resources Canada
  4. Department of Energy (DOE) - Geosciences [DE-FG02-92ER14244]
  5. DOE [DE-AC02-98CH10886]

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Variations in arsenic (As) mineralogy and geochemical controls on its mobility were evaluated in subsurface tailings at the historical Montague and Goldenville mine sites in Nova Scotia, Canada. Tailings at these sites contain some of the highest As concentrations in Nova Scotia and are located in close proximity to local communities. Pore water in the subsurface tailings is characterized by circumneutral to alkaline pH (6.2 to 8.7) and mildly reducing to oxidizing redox conditions (+130 mV to +347 mV). Bulk chemistry, scanning electron microscopy, and synchrotron micro-X-ray diffraction analyses showed As mineral hosts differ with depth. The deepest tailings (max. 2 m) are in direct contact with partially decomposed vegetation, which supports reducing conditions and the precipitation of authigenic As and Fe sulfides. Under reducing conditions, dissolved As concentrations are also controlled by desorption of As from dissolution of Fe and Mn oxides and the sorption or co-precipitation of As with carbonates. These geochemical controls differ from those influencing dissolved As concentrations under oxidizing conditions. In the near surface, As mobility is controlled by oxidative dissolution of primary arsenopyrite, precipitation of secondary Fe arsenates, Fe oxyhydroxides and Mn oxides, secondary Ca-Fe arsenates, and sorption onto Fe oxyhydroxides and gangue minerals. Some of these mineral species are stable under different conditions yet occur in close association, indicating the importance of microenvironments. The results of this study show that the weathering characteristics of these tailings vary with depth, leading to the formation of new As hosts that are distinct from those observed in the near surface. Identification of these As hosts provides an understanding of current controls on As mobility and has implications for future reprocessing and/or remediation efforts. (C) 2016 Elsevier Ltd. All rights reserved.

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