The Biogeochemistry of Indium, Gallium, and Germanium in Mine Wastes
Abstract
Indium (In), gallium (Ga), and germanium (Ge) are metals important in new energy technologies, and use of these metals is expanding dramatically. Humans are significantly impacting their natural cycling. Mining and smelting appear to be currently the largest sources of these metals to the environment, primarily because In, Ga, and Ge are byproducts of lead and zinc mining. The life cycle of these metals is poorly understood, including partitioning and speciation during mining processes, environmental behavior, and toxicity. The Tar Creek Superfund Site in Oklahoma, USA, is an abandoned Mississippi Valley-type lead and zinc mining area, containing sphalerite (ZnS) and galena (PbS). 30 major tailings piles remain in the area; elevated concentrations of lead (Pb), zinc (Zn), and cadmium (Cd) in these wastes have caused human health concerns. In order to better understand the biogeochemical cycling of In, Ga, and Ge associated with mining processes, we conducted geochemical and biological extractions of size-fractionated mine tailings from the Tar Creek site. Small tailings particles (<2.5 μm) contain higher concentrations of In, Ga, and Ge than large particles (>0.5 mm); a similar enrichment has been shown previously for Pb, Zn, and Cd. Ge is highly elevated in the mine wastes at this site; small particles contain up to 40x crustal concentrations. Ga and In are not significantly higher than crustal. (Crustal concentrations: Ge 1.4 mg/kg; Ga 14 mg/kg; In 100 mg/kg) While Pb, Zn, and Cd have been shown previously to be highly labile, and thus significantly re-worked from the original sulfide ore, sequential extractions suggest that In, Ga, and Ge are in less labile forms. In and Ga are liberated primarily from solutions that target semi-labile amorphous sulfides, Fe- and Mn-oxyhydroxides, and crystalline sulfide phases. By contrast, over 85% of the Ge in mine wastes from this site is bound in a residual mineral fraction (e.g. silicates) that is not liberated by a hot nitric acid leach. The bioaccessibility of In, Ga, and Ge also is significant - simulated gastric fluid extractions release 41-84% of each metal, suggesting that they do not reside in the ZnS or PbS phases. Future studies will further explore the cycling of Ga, Ge, and In at the Tar Creek site, including differences in speciation, mobility, and bioaccessibility of each.
- Publication:
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AGU Fall Meeting Abstracts
- Pub Date:
- December 2017
- Bibcode:
- 2017AGUFM.B13C1787W
- Keywords:
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- 0461 Metals;
- BIOGEOSCIENCES;
- 0489 Trace element cycling;
- BIOGEOSCIENCES;
- 1065 Major and trace element geochemistry;
- GEOCHEMISTRY;
- 1803 Anthropogenic effects;
- HYDROLOGY