Chalcopyrite-enargite concentrate primary resource
Mixed copper-sulfide mineral concentrates represented by the D3, Eb and Ea feeds in Oyama et al. (2021), distinct from the constituent chalcopyrite and enargite mineral species, the nearly pure model chalcopyrite tested separately in that paper, and the DC-I/DC-II/DC-III enargite-pyrite concentrates examined in Okibe et al. (2022). Figure 1 reports chalcopyrite/enargite/pyrite contents of 12/21/30 wt% for D3, 17/6.7/36 wt% for Eb and 8/24/10 wt% for Ea; bornite, chalcocite, geerite and other phases also occur. The displayed Ea phase labels total 97%, so the figure is not treated as a closed compositional balance. Mine, batch and beneficiation details are not established; the acknowledgments identify an academic supplier for Ea. This owner denotes concentrated geological feed, not a documented discarded residue, a pure phase or a traded product specification. No mineral identifier or constituent criticality designation is inherited.
Microbial & Biochemical Mechanisms (1)
Feed-dependent carbon-assisted mixed-culture copper dissolution
Associated Organisms:
Acidithiobacillus caldus (NCBITaxon:33059)
Laboratory inoculated concentrate assays showed feed-dependent associations between activated-carbon dose, solution redox trajectory and dissolved copper. For Eb, Section 3.2.1 reports day-30 soluble-copper fractions of 74%, 92% and 100% without carbon, with 0.05% w/v carbon and with 0.3% w/v carbon, respectively. For D3, the carbon-free curve plateaued just above 60%, whereas 0.05% carbon approached complete dissolution by day 35. For Ea, the carbon-free endpoint was reported as 54%; 0.3% carbon improved early dissolution but 0.05% gave the higher final soluble-copper outcome. These are source-reported mixed-feed dissolved fractions, referenced to copper in each feed, not isolated-metal yields or measured extraction of individual mineral phases. Parallel no-added-cell comparisons and evolving redox/pH profiles constrain the interpretation; the experiment does not establish a universal carbon optimum or a causal effect of the chalcopyrite/enargite ratio alone.
D3, Eb and Ea were used as received without washing or sterilization, with reported D50 values of 39, 81 and 49 micrometres. Duplicate 500 mL flasks contained 200 mL heterotrophic basal salts medium, 1% w/v feed, 5 mM ferrous iron supplied as ferrous sulfate, 0.01% w/v elemental sulfur and 0.01% w/v yeast extract. Initial medium pH was 1.5; sulfuric acid readjustment to 1.5 occurred on days 2 and 3 for D3 and day 4 for Eb, with no readjustment for Ea. Cultures were shaken aerobically at 45 degrees C and 150 rpm. Four source-labelled early-stationary-phase cultures, Acidiplasma sp. Fv-Ap, Acidimicrobium ferrooxidans ICP (DSM 10331), Sulfobacillus sibiricus N1 (DSM 17363) and Acidithiobacillus caldus KU (DSM 8584), were harvested, washed and introduced at 10^7 cells/mL each, 4 x 10^7 cells/mL total. The structured taxon names one verified species member only; no terminal community or member-specific causal census was performed. Powdered Wako activated carbon was reported as 46.5 micrometres and 1400 square metres/g; D3 received 0 or 0.05% w/v, and Eb/Ea 0, 0.05 or 0.3% w/v. Figure 6 covers approximately 30-35 days depending on feed, rather than a shared endpoint across all feeds. ICP-OES measured total soluble Cu, As and Fe; ferrous iron was measured separately and planktonic cells counted directly. Source-derived percentages are not an independently reconstructed sampling-corrected mass balance. Added iron and sulfur, variable phase assemblages, size, acid dosing and possible unmeasured reagent carryover limit cross-feed comparisons.
oyama_2021
oyama_2021
oyama_2021
oyama_2021
ncbi_caldus
okibe_2022
Sources & References
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oyama_2021: Oyama K, Takamatsu K, Hayashi K, Aoki Y, Kuroiwa S, Hirajima T and Okibe N (2021). Carbon-Assisted Bioleaching of Chalcopyrite and Three Chalcopyrite/Enargite-Bearing Complex Concentrates. Minerals 11(4):432, DOI 10.3390/min11040432. Complete official v2 PDF, 13 pages, Figures 1-6; original three-page supplement, Figures S1-S4. Sections 2.1-2.5 and 3.2 support the mixed-feed assays; model-mineral experiments are separate.
https://doi.org/10.3390/min11040432 (accessed 2026-10-12) -
ncbi_caldus: NCBI Taxonomy 33059, Acidithiobacillus caldus, species; type-strain aliases DSM 8584 and KU. Identifier context only, not authentication of the experimental stock or proof of one member's causal contribution.
https://www.ncbi.nlm.nih.gov/Taxonomy/Browser/wwwtax.cgi?id=33059&mode=Info (accessed 2026-10-12) -
okibe_2022: Okibe et al. (2022). Bioleaching of Enargite/Pyrite-Rich Dirty Concentrate and Arsenic Immobilization. Minerals 12(4):449, DOI 10.3390/min12040449. Sections 2-3, Table 1 and Figures 1-3; retained complete original inspected in the preceding curation and rechecked here for owner/experiment scope.
https://doi.org/10.3390/min12040449 (accessed 2026-10-12)
Curation History
| Timestamp | Curator | Action | Summary |
|---|---|---|---|
2026-10-12T11:44:52.561004Z |
Codex (GPT-6) | create | Created the distinct D3/Eb/Ea mixed-feed owner from complete official main and supplementary evidence, preserving control, quantitative, phase, version and experimental-overlap limits. |
Record source: data/records/chalcopyrite-enargite-concentrate.yaml