Iron-ore tailings secondary resource
Iron-ore tailings are processing-derived residual feeds from iron-ore production, distinct from natural iron ore, elemental iron and individual iron minerals. This record curates a mixed goethite/hematite/quartz tailing used as a source of biologically mobilized iron in a laboratory two-stage manganese-leaching experiment. The unnamed facility and tested composition do not define all iron-ore tailings. No criticality designation is inherited from constituents.
Microbial & Biochemical Mechanisms (1)
Mixed-culture iron mobilization from tailings for downstream manganese leaching
An anaerobic mixed-culture iron-tailings stage supplied Fe(II)-bearing liquor to a separate manganese-ore stage. The experiment supports iron mobilization from the mixed tailings in this culture system, consistent with the proposed reductive role of its dissolved iron. It does not quantify a particular organism or mineral phase contribution, or isolate a recovered iron product.
Living mixed metal-reducing cultures originated from a fen in Houghton County, Michigan, and previously adapted cultures inoculated the iron stage. No individual strain or causal community member is resolved here. Fermented Typha latifolia biomass plus 5 g/L sucrose supplied organic nutrient liquid. Methods 2.4 and Figure 5 describe two 250 mL Buechner flasks in series: the drawing labels 200 g iron feed and 350 g manganese ore. Methods 2.1 identifies the iron feed as tailings from an unnamed iron-ore production facility, smaller than 0.15 mm; the manganese ore came from an abandoned Keweenaw County mine and was crushed below 3 mm. After seven days of adaptation, 300 mL fresh nutrient per week was supplied in five 60 mL increments. Packed beds, fermentation locks and a submerged manganese-flask outlet were used to maintain anaerobic conditions. Experiments were run in triplicate. A numerical flask incubation temperature is not specified in these methods; Section 3.6 discusses ambient-temperature operation. Reported operating pH was 4.7 +/- 0.7 in the iron stage and 4.4 +/- 0.8 in the manganese stage. Overflow Mn was measured by colorimetric periodate oxidation and Fe(II) by 1,10-phenanthroline spectrophotometry; filtration and operational dissolved-fraction details are not supplied. These assays do not resolve the mineral phase contributing each metal.
borkar2026
borkar2026
borkar2026
borkar2026
Sources & References
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borkar2026: Borkar, Sharma, Rane, Boafo and Eisele (2026). Leaching of Manganese Using Bio-solubilized Iron Reductant to Prevent Manganese Carbonate Formation. Mining, Metallurgy & Exploration 43:2019–2030. DOI 10.1007/s42461-026-01506-2; Methods 2.1–2.6, Tables 1–7, Figures 5–13 and Results 3.1–3.6. Full 12-page primary article and figures inspected.
https://doi.org/10.1007/s42461-026-01506-2 (accessed 2026-10-11)
Curation History
| Timestamp | Curator | Action | Summary |
|---|---|---|---|
2026-10-11T11:42:56.094430+00:00 |
codex (GPT-6; codex) | CREATE | Created resource identity and narrowly scoped primary two-stage bioleaching evidence, preserving controls, analytical basis and scale limitations. |
Record source: data/records/iron-ore-tailings.yaml