CMMMech

Pentlandite mineral

Pentlandite is the (Ni,Fe)9S8 mineral species in the September 2026 IMA list. Status G denotes grandfathering and 1856 is an original-description year, not a sequential approval identifier. The species is distinct from elemental nickel, the nickel commodity, and impure sulfide ore or concentrate. The experiment below concerns an enriched pentlandite feed rather than an ideal single-phase solid. No constituent-element criticality is inherited.

Microbial & Biochemical Mechanisms (1)

Culture-associated nickel mobilization from enriched pentlandite at controlled pH

bioleaching Microbial

A living mixed acidophile culture enhanced nickel release from enriched pentlandite feed relative to uninoculated proton-leaching experiments in a laboratory pH-stat system. Inoculated nickel-release curves were similar at maintained pH 2 and 3, while dissolved iron was much lower at pH 3. Surface and solution analyses support coupled biological and chemical alteration; they do not demonstrate a unique enzyme pathway, member-specific causality, complete mineral conversion or a purified nickel product.

Experimental Context & Analytical Limits:
Sun et al. used Jinchuan material enriched by flotation and magnetic separation, reagent-cleaned, dried and ground below 0.074 mm. The feed contained 27.43 wt% Ni, 35.13 wt% Fe and 30.79 wt% S, with reported Cu, Mg, Co and Si impurities; it is not assumed to be pure pentlandite. A mixed culture from the National Engineering Laboratory of Biohydrometallurgy, Beijing, was reported initially dominated by Acidithiobacillus ferrooxidans, Ferrimicrobium acidiphilum and Leptospirillum ferrooxidans. No strain identifiers or member-specific activity tests were provided, so no taxon identifiers are assigned to the mixture. Cells grown in ferrous 9K medium were centrifuged in logarithmic growth to limit ionic carryover. The pH-stat assays used 8 g feed in 400 mL sterilized water in 500 mL vessels, 1.5 x 10^6 cells/mL, 33 degrees C and 250 rpm. Sulfuric acid and potassium bicarbonate maintained pH 2.00 or 3.00 within +/-0.05. The paper calls bioleaching tests duplicate but specifies one 8-day and one 16-day run, leaving independent 16-day replication and plotted error-bar meaning unresolved. Samples were taken every two days, filtered at 0.22 micrometre and analyzed by ICP-OES for Ni and total Fe, with Fe(II) titration, XRD, SEM and XPS of residues. Separately, ferric-ion experiments used 3 g feed per 100 mL, initial pH 1, 150 rpm and added kanamycin; those arms are not identical pH-stat microbial controls.
Curated Evidence Points:
Support Source: sun2020
Sections 2.2-2.3 and 3.2-3.3, Figures 9 and 12 show greater nickel release in the inoculated pH-stat experiments than in the abiotic proton-leaching series at the same pH setpoints, and similar inoculated nickel curves at pH 2 and 3. Figures 13-16 identify jarosite and sulfur-bearing residues and different surface species under the two pH conditions. These observations support conditional mineral-feed bioleaching; no values were digitized from graphs or represented as isolated recovery yields.
Partial Source: sun2020
The community profiles in Figure 17 are associations with residues, not proof of each named taxon's causal contribution. Figures 18-19 and Section 4 present a conceptual model; sulfur intermediates not detected by the assays and exact reaction equations are not independently established. pH control does not equal matched redox potential or ferric concentrations, and total acid/base addition or sample-volume correction is not reported. The 8-day/16-day design and undefined error bars limit quantitative reproducibility. Jarosite/sulfur accumulation and continuing nickel release do not prove that surface layers never inhibit leaching in other systems. Discussion of commercial heaps and possible magnesium selectivity is background or proposed application, not deployment or an industrial mass balance for this experiment.

Sources & References

  1. ima_2026_09: IMA-CNMNC. The New IMA List of Minerals, September 2026. PDF page 168, Pentlandite row; page 1, column definitions; page 2, distribution terms.
    https://cnmnc.units.it/files/editor/IMA_Master_List_(2026-09).pdf (accessed 2026-10-11)
  2. sun2020: Sun, Wen, Wu and Chen (2020). Mechanism for the Bio-Oxidation and Decomposition of Pentlandite: Implication for Nickel Bioleaching at Elevated pH. Minerals 10:289. DOI 10.3390/min10030289. Sections 2.1-2.3, 3.2-3.3, 4.2-4.4; Figures 9 and 12-17.
    https://doi.org/10.3390/min10030289 (accessed 2026-10-11)

Curation History

Timestamp Curator Action Summary
2026-10-11T09:02:00.252070+00:00 codex (GPT-6; codex) CREATE Created IMA-grounded pentlandite identity and qualified mixed-acidophile pH-stat bioleaching evidence.

Record source: data/records/pentlandite.yaml